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Title: A Treatise on Meteorological Instruments
       Explanatory of Their Scientific Principles, Method of
       Construction, and Practical Utility

Author: Henry Negretti
        Joseph Zambra

Release Date: June 18, 2011 [EBook #36457]

Language: English

Character set encoding: ASCII

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A TREATISE ON METEOROLOGICAL INSTRUMENTS.




  LONDON:
  PRINTED BY WILLIAMS AND STRAHAN,
  7 LAWRENCE LANE, CHEAPSIDE, E.C.




  A TREATISE ON METEOROLOGICAL INSTRUMENTS:

  EXPLANATORY OF

  THEIR SCIENTIFIC PRINCIPLES,
  METHOD OF CONSTRUCTION, AND PRACTICAL UTILITY.


  BY NEGRETTI & ZAMBRA,

  METEOROLOGICAL INSTRUMENT MAKERS TO THE QUEEN, THE ROYAL OBSERVATORY,
  GREENWICH, THE BRITISH METEOROLOGICAL SOCIETY, THE BRITISH AND FOREIGN
  GOVERNMENTS, ETC. ETC. ETC.


  LONDON:
  PUBLISHED AND SOLD AT NEGRETTI & ZAMBRA'S ESTABLISHMENTS:
  1 HATTON GARDEN, E.C., 59 CORNHILL, E.C., 122 REGENT STREET W.,
  AND 153 FLEET STREET, E.C.

  1864.

  _Price Five Shillings._




PREFACE.


The national utilisation of Meteorology in forewarning of storms, and the
increasing employment of instruments as weather indicators, render a
knowledge of their construction, principles, and practical uses necessary
to every well-informed person. Impressed with the idea that we shall be
supplying an existing want, and aiding materially the cause of
Meteorological Science, in giving a plain description of the various
instruments now in use, we have endeavoured, in the present volume, to
condense such information as is generally required regarding the
instruments used in Meteorology; the description of many of which could
only be found in elaborate scientific works, and then only briefly touched
upon. Every Meteorological Instrument now in use being fully described,
with adequate directions for using, the uninitiated will be enabled to
select those which seem to them best adapted to their requirements. With
accounts of old or obsolete instruments we have avoided troubling the
reader; on the other hand, we were unwilling to neglect those which,
though of no great practical importance, are still deserving of notice
from their being either novel or ingenious, or which, without being
strictly scientific, are in great demand as simple weather-glasses and
articles of trade.

We trust, therefore, that the work (however imperfect), bearing in mind
the importance of the subject, will be acceptable to general readers, as
well as to those for whose requirements it has been prepared.

The rapid progress made in the introduction of new apparatus of
acknowledged superiority has rendered the publication of some description
absolutely necessary. The Report of the Jurors for Class XIII. of the
International Exhibition, 1862, on Meteorological Instruments, fully bears
out our assertion, as shown by the following extract:--

"The progress in the English department has been very great;--in
barometers, thermometers, anemometers, and in every class of instruments.
At the close of the Exhibition of 1851, there seemed to have arisen a
general anxiety among the majority of makers to pay every attention to all
the essentials necessary for philosophical instruments, not only in their
old forms, but also with the view of obtaining other and better forms.
This desire has never ceased; and no better idea can be given of the
continued activity in these respects, than the number of patents taken out
for improvements in meteorological instruments in the interval between the
recent and preceding exhibitions, which amount to no less than forty-two."
* * * "In addition to numerous improvements patented by Messrs. Negretti
and Zambra, there is another of great importance, which they did not
patent, viz. enamelling the tubes of thermometers, enabling the makers to
use finer threads of mercury in the construction of all thermometers; for
the contrast between the opaque mercury and the enamel back of the tubes
is so great, that the finest bore or thread of mercury, which at one time
could not be seen without the greatest difficulty, is now seen with
facility; and throughout the British and Foreign departments, the makers
have availed themselves of this invention, the tubes of all being made
with enamelled backs. It is to be hoped that the recent exhibition will
give a fresh stimulus to the desire of improvement, and that the same rate
of progress will be continued."

To fulfil the desire of the International Jury in the latter portion of
the above extract will be the constant study of

NEGRETTI & ZAMBRA.

_1st January, 1864._




TABLE OF CONTENTS.


  CHAPTER I. INSTRUMENTS FOR ASCERTAINING THE ATMOSPHERIC PRESSURE.

  SECTION

  1. Principle of the Barometer.

  2. Construction of Barometers.

  3. Fortin's Barometer Cistern.

  4. STANDARD BAROMETER.

  5. Correction due to Capillarity.

  6.      "        "   Temperature.

  7.      "        "   Height.

  8. The Barometer Vernier.

  9. SELF-COMPENSATING STANDARD BAROMETER.

  10. BAROMETER WITH ELECTRICAL ADJUSTMENT.

  11. PEDIMENT BAROMETERS.

  12. The Words on the Scale.

  13. Correction due to Capacity of Cistern.

  14. PUBLIC BAROMETERS.

  15. FISHERY OR SEA-COAST BAROMETERS.

  16. Admiral FitzRoy's Words for the Scale.

  17. Instructions for Sea-coast Barometer.

  18. French Sea-coast Barometer.

  19. COMMON MARINE BAROMETER.

  20. THE KEW MARINE BAROMETER.

  21. Method of verifying Barometers.

  22. FITZROY'S MARINE BAROMETER.

  23. Words for its Scale.

  24. Trials of this Barometer under Gun-fire.

  25. NEGRETTI AND ZAMBRA'S FARMER'S BAROMETER AND DOMESTIC WEATHER-GLASS.

  26. Rules for Foretelling the Weather.

  27. Causes which may bring about a Fall or a Rise in the Barometer.

  28. Use of the Barometer in the Management of Mines.

  29. Use of the Barometer in estimating the Height of Tides.


  CHAPTER II. SYPHON TUBE BAROMETERS.

  30. Principle of.

  31. DIAL, OR WHEEL, BAROMETERS.

  32. STANDARD SYPHON BAROMETER.


  CHAPTER III. BAROGRAPHS, OR SELF-REGISTERING BAROMETERS.

  SECTION

  33. MILNE'S SELF-REGISTERING BAROMETER.

  34. MODIFICATION OF MILNE'S BAROMETER.

  35. KING'S SELF-REGISTERING BAROMETER.

  36. SYPHON, WITH PHOTOGRAPHIC REGISTRATION.


  CHAPTER IV. MOUNTAIN BAROMETERS.

  37. GAY LUSSAC'S MOUNTAIN BAROMETER.

  38. FORTIN'S MOUNTAIN BAROMETER.

  39. NEWMAN'S MOUNTAIN BAROMETER.

  40. NEGRETTI AND ZAMBRA'S PATENT MOUNTAIN AND OTHER BAROMETERS.

  41. Short Tube Barometer.

  42. Method of Calculating Heights by the Barometer; Tables and Examples.


  CHAPTER V. SECONDARY BAROMETERS.

  43. Desirability of Magnifying the Barometer Range.

  44. HOWSON'S LONG-RANGE BAROMETER.

  45. MCNEIL'S LONG-RANGE BAROMETER.

  46. The Water-glass Barometer.

  47. SYMPIESOMETERS.

  48. ANEROIDS.

  49. SMALL SIZE ANEROIDS.

  50. WATCH ANEROID.

  51. Measurement of Heights by the Aneroid; Example.

  52. METALLIC BAROMETER.


  CHAPTER VI. INSTRUMENTS FOR ASCERTAINING TEMPERATURE.

  53. Temperature.

  54. Thermometric Substances.

  55. Description of the Thermometer.

  56. STANDARD THERMOMETER.

  57. Method of ascertaining the exact Boiling Temperature; Tables, &c.

  58. Displacement of the Freezing Point.

  59. The Scale.

  60. The method of testing Thermometers.

  61. Porcelain Scale-Plates.

  62. Enamelled Tubes.

  63. THERMOMETERS OF EXTREME SENSITIVENESS.

  64. VARIETIES OF THERMOMETERS.

  65. SUPERHEATED STEAM THERMOMETER.

  66. THERMOMETER FOR SUGAR BOILING.

  67. EARTH THERMOMETER.

  68. MARINE THERMOMETER.


  CHAPTER VII. SELF-REGISTERING THERMOMETERS.

  69. Importance of.

  70. RUTHERFORD'S MAXIMUM THERMOMETER.

  71. PHILLIPS'S    DITTO    DITTO.

  72. NEGRETTI AND ZAMBRA'S PATENT MAXIMUM THERMOMETER.

  73. RUTHERFORD'S ALCOHOL MINIMUM THERMOMETER.

  74. HORTICULTURAL MINIMUM THERMOMETER.

  75. BAUDIN'S ALCOHOL MINIMUM THERMOMETER.

  76. Mercurial Minima Thermometers desirable.

  77. NEGRETTI AND ZAMBRA'S PATENT MERCURIAL MINIMUM THERMOMETER.

  78. NEGRETTI AND ZAMBRA'S SECOND PATENT MERCURIAL MINIMUM THERMOMETER.

  79. CASELLA'S PATENT MERCURIAL MINIMUM THERMOMETER.

  80. Day and Night Thermometer.

  81. SIXE'S SELF-REGISTERING THERMOMETER.


  CHAPTER VIII. RADIATION THERMOMETERS.

  82. Solar and Terrestrial Radiation considered.

  83. SOLAR RADIATION THERMOMETER.

  84. VACUUM SOLAR RADIATION THERMOMETER.

  85. TERRESTRIAL RADIATION THERMOMETER.

  86. AETHRIOSCOPE.

  87. PYRHELIOMETER.

  88. ACTINOMETER.


  CHAPTER IX. DEEP-SEA THERMOMETERS.

  89. ON SIXE'S PRINCIPLE.

  90. JOHNSON'S METALLIC THERMOMETER.


  CHAPTER X. BOILING-POINT THERMOMETERS.

  91. Ebullition.

  92. Relation between Boiling-Point and Elevation.

  93. HYPSOMETRIC APPARATUS.

  94. Precautions to ensure Correct Graduation.

  95. Method of Calculating Heights from Observations with the Mountain
      Thermometer; Example.

  96. THERMOMETERS FOR ENGINEERS.


  CHAPTER XI. INSTRUMENTS FOR ASCERTAINING THE HUMIDITY OF THE AIR.

  97. Hygrometric Substances.

  98. SAUSSURE'S HYGROMETER.

  99. Dew-Point.

  100. DROSOMETER.

  101. Humidity.

  102. LESLIE'S HYGROMETER.

  103. DANIEL'S HYGROMETER.

  104. REGNAULT'S CONDENSER HYGROMETER.

  105. Temperature of Evaporation.

  106. MASON'S HYGROMETER.

  107. SELF-REGISTERING HYGROMETER.

  108. Causes of Dew.

  109. Plan of Exposing Thermometers.


  CHAPTER XII. INSTRUMENTS USED FOR MEASURING THE RAINFALL.

  110. HOWARD'S RAIN-GAUGE.

  111. GLAISHER'S RAIN-GAUGE.

  112. RAIN-GAUGE WITH FLOAT.

  113. RAIN-GAUGE WITH SIDE TUBE.

  114. FITZROY'S RAIN-GAUGE.

  115. SELF-REGISTERING RAIN-GAUGE.

  116. The principle of Measurement.

  117. Position for Rain-gauge, &c.

  118. Cause of Rain.

  119. Laws of Rainfall.

  120. Utility of Statistics of Rainfall.

  121. NEW FORM OF RAIN-GAUGE.


  CHAPTER XIII. APPARATUS EMPLOYED FOR REGISTERING THE DIRECTION,
  PRESSURE, AND VELOCITY OF THE WIND.

  122. THE VANE.

  123. LIND'S WIND-GAUGE.

  124. HARRIS'S WIND-GAUGE.

  125. ROBINSON'S ANEMOMETER.

  126. WHEWELL'S ANEMOMETER.

  127. OSLER'S ANEMOMETER AND PLUVIOMETER.

  128. BECKLEY'S ANEMOMETER.

  129. SELF-REGISTERING WIND-GAUGE.

  130. Anemometric Observations.


  CHAPTER XIV. INSTRUMENTS FOR INVESTIGATING ATMOSPHERIC ELECTRICITY.

  131. ATMOSPHERIC ELECTROSCOPE.

  132. VOLTA'S ELECTROMETER.

  133. PELTIER'S ELECTROMETER.

  134. BOHNENBERGER'S ELECTROSCOPE.

  135. THOMSON'S ELECTROMETER.

  136. Fundamental Facts.

  137. Lightning Conductors.

  138. Precautions against Lightning.


  CHAPTER XV. OZONE AND ITS INDICATORS.

  139. Nature of Ozone.

  140. SCHONBEIN'S OZONOMETER.

  141. MOFFAT'S OZONOMETER.

  142. CLARK'S OZONE CAGE.

  143. Distribution and Effects of Ozone.

  144. LANCASTER'S REGISTERING OZONOMETER.


  CHAPTER XVI. MISCELLANEOUS INSTRUMENTS.

  145. CHEMICAL WEATHER GLASS.

  146. LESLIE'S DIFFERENTIAL THERMOMETER.

  147. ROMFORD'S DIFFERENTIAL THERMOMETER.

  148. GLAISHER'S THERMOMETER STAND.

  149. THERMOMETER SCREEN, FOR USE AT SEA.

  150. ANEMOSCOPE.

  151. EVAPORATING DISH, OR GAUGE.

  152. ADMIDOMETER.

  153. CLOUD REFLECTOR.

  154. SUNSHINE RECORDER.

  155. SET OF PORTABLE INSTRUMENTS.

  156. IMPLEMENTS.

  157. HYDROMETER.

  158. NEWMAN'S SELF-REGISTERING TIDE-GAUGE.




TABLES.


                                                                      PAGE

  Table of Corrections, for Capillary Depression of the Mercury
  in Boiled and in Unboiled Barometer-Tubes                              6

  Tables for Deducing Heights by means of the Barometer:--

    No. 1. Approximate Height due to Barometric Pressure                42

    No. 2. Correction for Mean Temperature of Air                       44

    No. 3. Correction due to Latitude                                   44

    No. 4. Correction due to Approximate Elevation                      45

  Tables for Determining the Temperature of the Vapour of Boiling
  Water at any Place:--

    No. 5. Factor due to Latitude                                       62

    No. 6. Temperature and Tension                                      62

  Table of Temperature of the Soil                                      69

  Table of Difference of Elevation corresponding to a fall of 1 deg.
  in the Boiling-point of Water                                         98

  Table showing Proportion of Salt for various Boiling Temperatures
  of Sea-Water                                                         100

  Table for finding the Degree of Humidity from Observations with
  Mason's Hygrometer                                                   108

  Table showing Amount and Duration of Rain at London, in 1862         112

  Table of Average British Rainfall in Westerly, Central, and
  Easterly districts                                                   114

  Table showing Force of Wind, for use with Lind's Wind-Gauge          118

  Tables for Correcting Observations made with--

    Brass Hydrometers                                                  142

    Glass Hydrometers                                                  143




ADDENDA.


                                                                      PAGE

  1. Rule for converting Millimetres into Inches, et vice versa        146

  2. Old French Lineal Measure, with English Equivalents               146

  3. Rule for finding Diameter of Bore of Barometer Tube               146

  4. Wind Scales                                                       147

  5. Letters to denote the State of the Weather                        147

  6. Table of Expansion of Bodies                                      148

  7. Table of Specific Gravity of Bodies                               148

  8. Important Temperatures                                            148

  9. Table of Meteorological Elements, forming Exponents of the
  Climate of London                                                    149

  10. List of Works on Meteorology                                     151




METEOROLOGICAL INSTRUMENTS.


In the pursuits and investigations of the science of Meteorology, which is
essentially a science of observation and experiment, instruments are
required for ascertaining, 1. the pressure of the atmosphere at any time
or place; 2. the temperature of the air; 3. the absorption and radiation
of the sun's heat by the earth's surface; 4. the humidity of the air; 5.
the amount and duration of rainfall; 6. the direction, the horizontal
pressure, and the velocity of winds; 7. the electric condition of the
atmosphere, and the prevalence and activity of ozone.




CHAPTER I.

INSTRUMENTS FOR ASCERTAINING THE ATMOSPHERIC PRESSURE.


[Illustration: Fig. 1.]

=1. Principle of the Barometer.=--The first instrument which gave the
exact measure of the pressure of the atmosphere was invented by
Torricelli, in 1643. It is constructed as follows:--A glass tube, CD (fig.
1), about 34 inches long, and from two to four-tenths of an inch in
diameter of bore, having one end closed, is filled with mercury. In a cup,
B, a quantity of mercury is also poured. Then, placing a finger securely
over the open end, C, invert the tube vertically over the cup, and remove
the finger when the end of the tube dips into the mercury. The mercury in
the tube then partly falls out, but a column, AB, about 30 inches in
height, remains supported. This column is a weight of mercury, the
pressure of which upon the surface of that in the cup is precisely
equivalent to the corresponding pressure of the atmosphere which would be
exerted in its place if the tube were removed. As the atmospheric pressure
varies, the length of this mercurial column also changes. It is by no
means constant in its height; in fact, it is very seldom stationary, but
is constantly rising or falling through a certain extent of the tube, at
the level of the sea, near which the above experiment is supposed to be
performed. It is, therefore, an instrument by which the fluctuations
taking place in the pressure of the atmosphere, arising from changes in
its weight and elasticity, can be shown and measured. It has obtained the
name _Barometer_, or measurer of heaviness,--a word certainly not happily
expressive of the utility of the invention. If the bore of the barometer
tube be uniform throughout its length, and have its sectional area equal
to a square inch, it is evident that the length of the column, which is
supported by the pressure of the air, expresses the number of cubic inches
of mercury which compose it. The weight of this mercury, therefore,
represents the statical pressure of the atmosphere upon a square inch of
surface. In England the annual mean height of the barometric column,
reduced to the sea-level and to the temperature of 32 deg. Fahrenheit, is
about 29.95 inches. A cubic inch of mercury at this temperature has been
ascertained to weigh 0.48967 lbs. avoirdupois. Hence, 29.95 x 0.48967=
14.67 lbs., is the mean value of the pressure of the atmosphere on each
square inch of surface, near the sea-level, about the latitude of 50
degrees. Nearer the equator this mean pressure is somewhat greater; nearer
the poles, somewhat less. For common practical calculations it is assumed
to be 15 lbs. on the square inch. When it became apparent that the
movements of the barometric column furnished indications of the probable
coming changes in the weather, an attempt was made to deduce from recorded
observations the barometric height corresponding to the most notable
characteristics of weather. It was found that for fine dry weather the
mercury in the barometer at the sea-level generally stood above 30 inches;
changeable weather happened when it ranged from 30 to 29 inches, and when
rainy or stormy weather occurred it was even lower. Hence, it became the
practice to place upon barometer scales words indicatory of the weather
likely to accompany, or follow, the movements of the mercury; whence the
instruments bearing them obtained the name "Weather Glasses."


=2. Construction of Barometers.=--In order that the instrument may be
portable, it must be made a fixture and mounted on a support; and,
further, to render it scientifically or even practically useful, many
precautions are required in its construction. The following remarks apply
to the construction of all barometers:--Mercury is universally employed,
because it is the heaviest of fluids, and therefore measures the
atmospheric pressure by the shortest column. Water barometers have been
constructed, and they require to be at least 34 feet long. Oil, or other
fluids, might be used. Mercury, however, has other advantages: it has
feeble volatility, and does not adhere to glass, if pure. Oxidised, or
otherwise impure mercury, may adhere to glass; moreover, such mercury
would not have the density of the pure metal, and therefore the barometric
column would be either greater or less than it should be. The mercury of
commerce generally contains lead; sometimes traces of iron and sulphur. It
is necessary, therefore, for the manufacturer to purify the mercury; and
this is done by washing it with diluted acetic, or sulphuric acid, which
dissolves the impurities. No better test can be found for ascertaining if
the mercury be pure than that of filling a delicate thermometer tube; if,
on exhausting the air from this thermometer, the mercury will freely run
up and down the bore, which is probably one thousandth of an inch in
diameter, the mercury from which this thermometer was made will be found
fit for any purpose, and with it a tube may be filled and boiled, not only
of one inch, but even of two inches diameter. In all barometers it is
requisite that the space above the mercurial column should be completely
void of air and aqueous vapour, because these gases, by virtue of their
elasticity, would depress the column. To exclude these the mercury is
introduced, and boiled in the tube, over a charcoal fire, kept up for the
purpose. In this manner the air and vapour which adhere to the glass are
expanded, and escape away. One can tell whether a barometer has been
properly "boiled," as it is termed, by simply holding the tube in a
slanting direction and allowing the mercury to strike the top. If the
boiling has been well performed, the mercury will give a clear, metallic
sound; if not, a dull, flat sound, showing some air to be present.

When the mercury in a barometer tube rises or falls, the level of the
mercury in the cup, or _cistern_, as it is generally termed, falls or
rises by a proportionate quantity, which depends upon the relative areas
of the interior of the tube and of the cistern. It is necessary that this
should be taken into consideration in ascertaining the exact height of the
column. If a fixed scale is applied to the tube, the correct height may be
obtained by applying a correction for capacity. A certain height of the
mercury is ascertained to be accurately measured by the scale, and should
be marked on the instrument as the _neutral point_. Above this point the
heights measured are all less, and below, all more, than they should be.
The ratio between the internal diameters of the tube and cistern (which
should also be stated on the instrument, as, for instance, capac. 1/50)
supplies the data for finding the correction to be applied. This
correction is obviated by constructing the cistern so as to allow of the
surface of the mercury in it being adjustable to the commencement of the
fixed scale, as by Fortin's or Negretti's plan. It is also unnecessary in
barometers constructed on what is now called the "Kew method." These will
all be detailed in their proper place. The tube, being fixed to the
cistern, may have a moveable scale applied to it. But such an arrangement
requires the utmost care and skill in observing, and is seldom seen except
in first-class Observatories.


[Illustration: Fig. 2.]

=3. Fortin's Barometer.=--Fortin's plan of constructing a barometer
cistern is shown in fig. 2. The cistern is formed of a glass cylinder,
which allows of the level of the mercury within being seen. The bottom of
the cylinder is made of sheep-skin or leather, like a bag, so as to allow
of being pushed up or lowered by means of a screw, D B, worked from
beneath. This screw moves through the bottom of a brass cylinder, C C,
which is fixed outside, and protects the glass cylinder containing the
mercury. At the top of the interior of the cistern is fixed a small piece
of ivory, A, the point of which exactly coincides with the zero of the
scale. This screw and moveable cistern-bottom serve also to render the
barometer portable, by confining the mercury in the tube, and preventing
its coming into the cistern, which is thus made too small to receive it.


4. STANDARD BAROMETER.

Fig. 3 represents a Standard Barometer on Fortin's principle. The
barometer tube is enclosed and protected by a tube of brass extending
throughout its whole length; the upper portion of the brass tube has two
longitudinal openings opposite each other; on one side of the front
opening is the barometrical scale of English inches, divided to show, by
means of a vernier, 1/500th of an inch; on the opposite side is sometimes
divided a scale of French millimetres, reading also by a vernier to 1/10th
of a millimetre (see directions for reading the vernier, page 7). A
thermometer, C, is attached to the frame, and divided to degrees, which
can be read to tenths; it is necessary for ascertaining the temperature of
the instrument, in order to correct the observed height of the barometer.

[Illustration: Fig. 3.]

As received by the observer, the barometer will consist of two parts,
packed separately for safety in carriage,--1st, the barometer tube and
cistern, filled with mercury, the brass tube, with its divided scale and
thermometer; and 2nd, a mahogany board, with bracket at top, and brass
ring with three adjusting screws at bottom.

_Directions for fixing the Barometer._--In selecting a position for a
barometer, care should be taken to place it so that the sun cannot shine
upon it, and that it is not affected by direct heat from a fire. The
cistern should be from two to three feet above the ground, which will give
a height for observing convenient to most persons. A standard barometer
should be compared with an observatory standard of acknowledged accuracy,
to determine its index error; which, as such instruments are graduated by
micrometrical apparatus of great exactitude, will be constant for all
parts of the scale. It should be capable of turning on its axis by a
movement of the hand, so that little difficulty can ever be experienced in
obtaining a good light for observation. Having determined upon the
position in which to place the instrument, fix the mahogany board as
nearly vertical as possible, and ascertain if the barometer is perfect and
free from air, in the following manner:--lower the screw at the bottom of
the cistern several turns, so that the mercury in the tube, when held
upright, may fall two or three inches from the top; then slightly incline
the instrument from the vertical position, and if the mercury in striking
the top elicit a sharp tap, the instrument is perfect. Supposing the
barometer to be in perfect condition, as it is almost sure to be, it is
next suspended on the brass bracket, its cistern passing through the ring
at bottom, and allowed to find its vertical position, after which it is
firmly clamped by means of the three thumb-screws.

_To Remove the Instrument when fixed to another Position._--If it should
be necessary to remove the barometer,--first, by means of the adjusting
screw, drive the mercury to the top of the tube, turning it gently when it
is approaching the top, and cease directly any resistance is experienced;
next, remove from the upper bracket or socket; lift the instrument and
invert it, carrying it with its lower end upwards.

_Directions for taking an Observation._--Before making an observation, the
mercury in the cistern must be raised or lowered by means of the
thumb-screw, F, until the ivory point, E, and its reflected image in the
mercury, D, are just in contact; the vernier is then moved by means of the
milled head, until its lower termination just excludes the light from the
top of the mercurial column; the reading is then taken by means of the
scale on the limb and the vernier. The vernier should be made to read
upward in all barometers, unless for a special object, as this arrangement
admits of the most exact setting. In observing, the eye should be placed
in a right line with the fore and back edges of the lower termination of
the vernier; and this line should be made to form a tangent to the apex of
the mercurial column. A small reflector placed behind the vernier and
moving with it, so as to assist in throwing the light through the back
slit of the brass frame on to the glass tube, is advantageous; and the
observer's vision may be further assisted by the aid of a reading lens.
The object is, in these Standard Barometers, to obtain an exact reading,
which can only be done by having the eye, the fore part of the zero edge
of the vernier, the top of the mercurial column, and the back of the
vernier, in the same horizontal plane.

_Uniformity of Calibre._--The diameter of that part of the tube through
which the oscillations of the mercury will take place is very carefully
examined to insure uniformity of calibre, and only those tubes are used
which are as nearly as possible of the same diameter throughout. The size
of the bore should be marked on the frame of the barometer in tenths and
hundredths of an inch. A correction due to capillary action, and depending
on the size of the tube, must be applied to the readings.


=5. Correction due to Capillarity.=--When an open tube of small bore is
plunged into mercury, the fluid will not rise to the same level inside as
it has outside. Hence, the effect of capillary action is to depress the
mercurial column; and the more so the smaller the tube. The following
table gives the correction for tubes in ordinary use:--

  Diameter     Depression, in     Depression, in
  of tube.     boiled tubes.      unboiled tubes.
   INCH.          INCH.               INCH.

   0.60           0.002               0.004
   0.55           0.003               0.005
   0.50           0.003               0.007
   0.45           0.005               0.010
   0.40           0.007               0.015
   0.35           0.010               0.021
   0.15           0.044               0.029
   0.10           0.070               0.041
   0.30           0.014               0.058
   0.25           0.020               0.086
   0.20           0.029               0.140

This correction is always additive to the observed reading of the
barometer.


=6. Correction due to Temperature.=--In all kinds of mercurial barometers
attention must be given to the temperature of the mercury. As this metal
expands and contracts very much for variations of temperature, its density
alters correspondingly, and in consequence the height of the barometric
column also varies. To ascertain the temperature of the mercury, a
thermometer is placed near the tube, and is sometimes made to dip into the
mercury in the cistern. The freezing point of water, 32 deg.F., is the
temperature to which all readings of barometers must be reduced, in order
to make them fairly comparable. The reduction may be effected by
calculation, but the practical method is by tables for the purpose; and
for these tables we refer the reader to the works mentioned at the end of
this book.


=7. Correction due to Height above the Half-tide Level.=--Further, in
order that barometrical observations generally may be made under similar
circumstances, the readings, corrected for capacity, capillarity, and
temperature, should be reduced to what they would be at the sea-level, by
adding a correction corresponding to the height above the mean level of
the sea, or of half-tide. For practical purposes of comparison with
barometric pressure at other localities, add one-tenth of an inch to the
reading for each hundred feet of elevation above the sea. For scientific
accuracy this will not suffice, but a correction must be obtained by means
of Schuckburg's formula, or tables computed therefrom.


=8. The Barometer Vernier.=--The _vernier_, an invaluable contrivance for
measuring small spaces, was invented by Peter Vernier, about the year
1630. The barometer scale is divided into inches and tenths. The vernier
enables us to accurately subdivide the tenths into hundredths, and, in
first-class instruments, even to thousandths of an inch. It consists of a
short scale made to pass along the graduated fixed scale by a sliding
motion, or preferably by a rack-and-pinion motion, the vernier being fixed
on the rack, which is moved by turning the milled head of the pinion. The
principle of the vernier, to whatever instrumental scale applied, is that
the divisions of the moveable scale are to those in an equal length of the
fixed scale in the proportion of two numbers which differ from each other
by unity.

[Illustration: Fig. 4.]

[Illustration: Fig. 5.]

The scales of standard barometers are usually divided into half-tenths, or
.05, of an inch, as represented, in fig. 5, by AB. The vernier, CD, is
made equal in length to twenty-four of these divisions, and divided into
twenty-five equal parts; consequently one space on the scale is larger
than one on the vernier by the twenty-fifth part of .05, which is .002
inch, so that such a vernier shows differences of .002 inch. The vernier
of the figure reading upwards, the lower edge, D, will denote the top of
the barometer column; and is the zero of the vernier scale. In fig. 4, the
zero being in line exactly with 29 inches and five-tenths of the fixed
scale, the barometer reading would be 29.500 inches. It will be seen that
the vernier line, _a_, falls short of a division of the scale by, as we
have explained, .002 inch; _b_, by .004; _c_, by .006; _d_, by .008; and
the next line by one hundredth. If, then, the vernier be moved so as to
make _a_ coincide with _z_, on the scale, it will have moved through .002
inch; and if 1 on the vernier be moved into line with _y_ on the scale,
the space measured will be .010. Hence, the figures 1, 2, 3, 4, 5 on the
vernier measure hundredths, and the intermediate lines even thousandths of
an inch. In fig. 5, the zero of the vernier is intermediate 29.65 and
29.70 on the scale. Passing the eye up the vernier and scale, the second
line above 3 is perceived to lie evenly with a line of the scale. This
gives .03 and .004 to add to 29.65, so that the actual reading is 29.684
inches. It may happen that no line on the vernier _accurately_ lies in the
same straight line with one on the scale; in such a case a doubt will
arise as to the selection of one from two equally coincident, and the
intermediate thousandth of an inch should be taken.

For the ordinary purposes of the barometer as a "weather-glass," such
minute measurement is not required. Hence, in household and marine
barometers the scale need only be divided to tenths, and the vernier
constructed to measure hundredths of an inch. This is done by making the
vernier either 9 or 11-10ths of an inch long, and dividing it into ten
equal parts. The lines above the zero line are then numbered from 1 to 10;
sometimes the alternate divisions only are numbered, the intermediate
numbers being very readily inferred. Hence, if the first line of the
vernier agrees with one on the scale, the next must be out one-tenth of a
tenth, or .01 of an inch from agreement with the next _scale_ line; the
following vernier line must be .02 out, and so on. Consequently, when the
vernier is set to the mercurial column, the difference shown by the
vernier from the tenth on the scale is the hundredths to be added to the
inches and tenths of the scale.

A little practice will accustom a person to set and read any barometer
quickly; an important matter where accuracy is required, as the heat of
the body, or the hand, is very rapidly communicated to the instrument, and
may vitiate, to some extent, the observation.


9. SELF-COMPENSATING STANDARD BAROMETER.

This barometer has been suggested to Messrs. Negretti and Zambra by
Wentworth Erk, Esq. It consists of a regular barometer; but attached to
the vernier is a double rack worked with one pinion, so that in setting or
adjusting the vernier in one position, the second rack moves in directly
the opposite direction, carrying along with it a plug or plunger the exact
size of the internal diameter of the tube dipping in the cistern, so that
whatever the displacement that has taken place in the cistern, owing to
the rise or fall of the mercury, it is exactly compensated by the plug
being more or less immersed in the mercury, so that no capacity correction
is required.

A barometer on this principle is, however, no novelty, for at the Royal
Society's room a very old instrument may be seen reading somewhat after
the same manner.

[Illustration: Fig. 6.]

Fig. 6 is an illustration of the appearance of this instrument. The
cistern is so constructed that the greatest amount of light is admitted to
the surface of the mercury.


10. BAROMETER WITH ELECTRICAL ADJUSTMENT.

This barometer is useful to persons whose eyesight may be defective; and
is capable of being read off to greater accuracy than ordinary barometers,
as will be seen by the following description:--The barometer consists of
an upright tube dipping into a cistern, so contrived, that an up-and-down
movement, by means of a screw, can be imparted to it. In the top of the
tube a piece of platina wire is hermetically sealed. The cistern also has
a metallic connection, so that by means of covered copper wires (in the
back of the frame) a circuit is established; another connection also
exists by means of a metallic point dipping into the cistern. The circuit,
however, can be cut off from this by means of a switch placed about midway
up the frame; on one side of the tube is placed a scale of inches; a small
circular vernier, divided into 100 parts, is connected with the dipping
point, and works at right angles with this scale.

To set the instrument in action for taking an observation, a small battery
is connected by means of two small binding screws at the bottom of the
frame. The switch is turned upwards, thereby disconnecting the dipping
point; the cistern is then screwed up, so that the mercury in the tube is
brought into contact with the platina wire at the top; the instant this is
effected the magnetic needle seen on the barometer will be deflected. The
switch is now turned down; by so doing the connection with the upper wire
or platina is cut off, and established instead only between the dipping
point carrying the circular vernier and the bottom of the cistern; the
point is now screwed by means of the milled head until the needle is again
deflected. We may now be sure that the line on the circular vernier that
cuts the division on the scale is the exact height of the barometer.
Although the description here given may seem somewhat lengthy, the
operation itself is performed in less time than would be taken in reading
off an ordinary instrument.


11. PEDIMENT BAROMETERS.

[Illustration: Fig. 7.]

[Illustration: Fig. 8.]

[Illustration: Fig. 9.]

[Illustration: Fig. 10.]

[Illustration: Fig. 11.]

These Barometers, generally for household purposes, are illustrated by
figs. 7 to 11. They are intended chiefly for "weather glasses," and are
manufactured to serve not only a useful, but an ornamental purpose as
well. They are usually framed in wood, such as mahogany, rosewood, ebony,
oak or walnut, and can be obtained either plain or handsomely and
elaborately carved and embellished, in a variety of designs, so as to be
suitable for private rooms, large halls, or public buildings. The scales
to the barometer and its attached thermometer may be ivory, porcelain, or
silvered metal. It is not desirable that the vernier should read nearer
than one-hundredth of an inch. Two verniers and scales may be fitted one
on either side of the mercurial column, so that one can denote the last
reading, and thus show at a glance the extent of rise or fall in the
interval. The scale and thermometer should be covered with plate glass. A
cheap instrument has an open face and plain frame, with sliding vernier
instead of rack-and-pinion motion. The barometer may or may not have a
moveable bottom to the cistern, with screw for the purpose of securing the
mercury for portability. The cistern should not, however, require
adjustment to a zero or fiducial point. It should be large enough to
contain the mercury, which falls from 31 to 27 inches, without any
appreciable error on the height read off on the scale.


=12. The Words on the Scale.=--The following words are usually engraved on
the scales of these barometers, although they are not now considered of so
much importance as formerly:--

  At 31  inches         Very dry.
  "  30.5  "            Settled fair.
  "  30    "            Fair.
  "  29.5  "            Changeable.
  "  29    "            Rain.
  "  28.5  "            Much rain.
  "  28    "            Stormy.

The French place upon their barometers a similar formula:--

  At 785 millimetres    Tres-sec.
  "  776      "         Beau-fixe.
  "  767      "         Beau temps.
  "  758      "         Variable.
  "  749      "         Pluie ou vent.
  "  740      "         Grande pluie.
  "  731      "         Tempete.

Manufacturers of barometers have uniformly adopted these indications for
all countries, without regard to the elevation above the sea, or the
different geographical conditions; and as it can readily be shown that the
height and variations of the barometer are dependent on these, it follows
that barometers have furnished indications which, under many
circumstances, have been completely false. Even in this country, and near
the sea-level, storms are frequent with the barometer not below 29; rain
is not uncommon with the glass at 30; even fine weather sometimes occurs
with a low pressure; while it is evident that at an elevation of a few
thousand feet the mercury would never rise to 30 inches; hence, according
to the scale, there should never be fair weather there. If tempests
happened as seldom in our latitude as the barometer gets down to 28
inches, the maritime portion of the community at least would be happy
indeed. These words have long been ridiculed by persons acquainted with
the causes of the barometric fluctuations; nevertheless opticians continue
to place them on the scales, evidently only because they appear to add to
the importance of the instrument in the eyes of those who have not learned
their general inutility. In different regions of the world, the
indications of the barometer are modified by the conditions peculiar to
the geographical position and elevation above the sea, and it is necessary
to take account of these in any attempt to found rules of general utility
in connection with the barometer as a weather guide. All that can be said
in favour of these words is, that within a few hundred feet of the
sea-level, when the column rises or falls gradually during two or three
days towards "Fair" or "Rain," the indications they afford of the coming
weather are generally extremely probable; but when the variations are
quick, upward or downward, they presage unsettled or stormy weather.

Admiral FitzRoy writes:--"The words on the scales of barometers should not
be so much regarded, for weather indications, as the rising or falling of
the mercury; for if it stands at _Changeable_, and then rises a little
towards _Fair_, it presages a change of wind or weather, though not so
great as if the mercury had risen higher; and, on the contrary, if the
mercury stands above _Fair_ and falls, it presages a change, though not to
so great a degree as if it had stood lower; besides which, the direction
and force of wind are not in any way noticed. It is not from the point at
which the mercury stands that we are alone to form a judgment of the state
of the weather, but from its _rising_ or _falling_; and from the movements
of immediately preceding days as well as hours, keeping in mind effects of
change of _direction_ and dryness, or moisture, as well as alteration of
force or strength of wind."[1]


=13. Correction due to Capacity of Cistern.=--These barometers, having no
adjustment for the zero of the scale, require a correction for the varying
level of the mercury in the cistern, when the observations are required
for strict comparison with other barometric observations, or when they are
registered for scientific purposes; but for the common purpose of
predicting the weather, this correction is unnecessary. The neutral point,
and the ratio of the bore of the tube to the diameter of the cistern, must
be known (see p. 3). Then the capacity correction, as it is termed, is
found as follows:--Take the fractional part, expressed by the capacity
ratio, of the difference between the observed reading and the height of
the neutral point; then, if the mercury stand _below_ the neutral point,
_subtract_ this result from the reading; if it stand _above_, _add_ it to
the reading.

For example, suppose the neutral point to be 29.95 inches, and the
capacity ratio 1/50, required the correction when the barometer reads
30.78.

  Here                  30.78 - 29.95 = 0.83
  Correction                = 0.83/50 = +0.02 nearly.
  Scale reading                         30.78
                                        -----
  Correct reading                       30.80
                                        =====

Of course the correction could as easily be found to three decimal places,
if desirable. It is evident that the correction is more important the
greater the distance of the top of the mercury from the neutral point.


14. PUBLIC BAROMETERS.

Since the increased attention paid to the signs of forthcoming weather of
late years, and the good which has resulted therefrom to farmers,
gardeners, civil engineers, miners, fishermen, and mariners generally, by
forewarning of impending wet or stormy weather, the desirability of having
good barometers exposed in public localities has become evident.

Barometers may now be seen attached to drinking fountains, properly
protected, and are frequently consulted by the passers-by. But it is among
those whose lives are endangered by sudden changes in the weather,
fishermen especially, that the warning monitor is most urgently required.
Many poor fishing villages and towns have therefore been provided by the
Board of Trade, at the public expense, and through the humane effort of
Admiral FitzRoy, with first-class barometers, each fixed in a conspicuous
position, so as to be easily accessible to all who desire to consult it.
Following this example, the Royal National Life Boat Institution has
supplied each of its stations with a similar storm warner; the Duke of
Northumberland and the British Meteorological Society have erected several
on the coast of Northumberland; and many other individuals have presented
barometers to maritime places with which they are connected.

These barometers have all been manufactured by Messrs. Negretti and
Zambra. The form given to the instrument seems well adapted for public
purposes.


[Illustration: Fig. 12.]

=15. Fishery or Sea-coast Barometers.=--Fig. 12 gives a representation of
these coast and fishery barometers. The frame is of solid oak, firmly
screwed together. The scales are very legibly engraved on porcelain by
Negretti and Zambra's patent process. The thermometer is large, and easily
read; and as this instrument is exposed, it will indicate the actual
temperature sufficiently for practical purposes. The barometer tube is
three-tenths of an inch in diameter of bore, exhibiting a good column of
mercury; and the cistern is of such capacity, in relation to the tube,
that the change of height in the surface of the mercury in the cistern
corresponding to a change of height of three inches of mercury in the
tube, is less than one-hundredth of an inch, and therefore, as the
readings are only to be made to this degree of accuracy, this small error
is of no importance. The cistern is made of boxwood, which is sufficiently
porous to allow the atmosphere to influence the mercurial column; but the
top is plugged with porous cane, to admit of free and certain play.


=16. Admiral FitzRoy's Scale Words.=--The directions given on the scales
of these barometers were drawn up by Admiral FitzRoy, F.R.S. They appear
to be founded on the following considerations:--

Supposing a compass diagram, with the principal points laid down, the N.E.
is the wind for which the barometer stands highest; for the S.W. wind it
is lowest. This is found to be so in the great majority of cases; but
there are exceptions to this, as to all rules. The N.E. and S.W. may
therefore be regarded as the poles of the winds, being opposite each
other. When the wind veers from the S.W. through W. and N. to N.E., the
barometer gradually rises; on the contrary, when the wind veers from N.E.
and E. to S.E., S. and S.W., the mercury falls. A similar curious law
exists in relation to the veering of the wind, and the action of the
thermometer. As the wind veers from the S.W. to W. and N., the thermometer
falls; as it veers from N.E. to E. and S., it rises, because the wind gets
from a colder to a warmer quarter. The polar winds are cold, dry, and
heavy. Those from the equatorial regions are warm, moist, and
comparatively light.

These laws have been clearly developed and expressed by Professor Dove in
his work on the "Law of Storms." The warm winds of Europe are those which
bring the greatest quantity of rain, as they blow from the ocean, and come
heavily laden with moisture. The cold winds, besides containing less
moisture, blow more from the land. The weight of the vapour of the warm
winds tends to raise the barometric column; but, at the same time, the
increased dilatation of the air tends to lower it. This latter influence
being the stronger, the barometer always falls for these winds; and in
regions where they traverse a large extent of land, retain their heat, and
become necessarily very dry, the fall in the barometer will be greater.
Admiral FitzRoy's words for the scales of barometers for use in northern
latitudes, then, are as follows:--

    _RISE._                      _FALL._
      FOR                          FOR
    N. ELY.                      S. WLY.
  NW.--N.--E.                  SE.--S.--W.
      DRY                          WET
      OR                           OR
     LESS                         MORE
     WIND.                        WIND.
   -------                      -------
    EXCEPT                       EXCEPT
   WET FROM                     WET FROM
    N. ED.                       N. ED.
   -------                      -------
  Long foretold, long last;    First rise after low,
  Short notice, soon past.     Foretells stronger blow.

It will be perceived that the exception in each case applies to N.E.
winds. The barometer may fall with north-easterly winds, but they will be
violent and accompanied with rain, hail, or snow; again, it will rise with
these winds accompanied with rain, when they are light, and bring only
little rain. It rises, however, highest with the dry and light N.E. winds.

These directions are very practically useful; they provide for
geographical position--also for elevation above the sea--since they are
not appended to any particular height of the column. They are suited to
the northern hemisphere generally, as well as around the British Isles.
The same directions are adapted to the southern hemisphere, by simply
substituting for the letter N the letter S, reading south for north, and
_vice versa_. South of the equator the cold winds come from the south; the
warm, from the north. The S.E. wind in the southern hemisphere corresponds
to the N.E. in the northern. The laws there are, while the wind veers from
S.E. through E. to N. and N.W., the barometer falls and the thermometer
rises. As the wind veers from N.W. through W. and S. to S.E., the
barometer rises and the thermometer falls.


=17. Instructions for the Sea-coast Barometer.=--The directions for fixing
the barometer, and making it portable when it has to be removed, should be
attended to carefully. The barometer should be suspended against a frame
or piece of wood, so that light may be seen _through_ the tube. Otherwise
a piece of paper, or a _white place_, should be behind the upper or _scale
part_ of the _tube_.

When suspended on a hook, or stout nail, apply the milled-head key (which
will be found just below the scales) to the square brass pin at the lower
end of the instrument, and turn _gently_ toward the left hand till the
screw stops; then take off the key and replace it for use, near the scale,
as it was before. The cistern bottom being thus _let down_, the mercury
will sink to its proper level quickly.

In removing this barometer it is necessary to _slope it gradually_, till
the mercury is at the top of the tube, and then, with the instrument
reversed, to screw up the cistern bottom, or bag, by the key, used
_gently_, till it stops. It will then be portable, and may be carried with
the _cistern_ end _upwards_, or lying flat; but it must not be jarred, or
receive a concussion.


=18. French Sea-coast Barometer.=--The French have imitated this form of
barometer for coast service, and have translated Admiral FitzRoy's
indications for the scale as follows:--

          LA                            LA
        HAUSSE                        BAISSE
       INDIQUE.                      INDIQUE.
       ---------                     ---------
    DES VENTS DE LA               DES VENTS DE LA
       PARTIE DU                     PARTIE DU
          N.E.                          S.O.
    (DU N.O. a l'E)               (DU S.E. a l'O.)
    (PAR LE NORD. )               (PAR LE SUD.   )
        DE LA                            DE
      SECHERESSE.                   L'HUMIDITE.
       ---------                     ---------
        UN VENT                       UN VENT
      PLUS FAIBLE                    PLUS FORT
   EXCEPTE S'IL PLEUT            EXCEPTE S'IL PLEUT
  AVEC DE FORTES BRISES        AVEC DE PETITES BRISES
        DU N.E.                       DU N.E.
       ---------                     ---------
    Mouvements lents,             Le commencement
     Temps durable.                de la hausse,
       ---------                  apres une grande
   Mouvements rapides,             baisse presage
    Temps variable.               un Vent violent.


MARINE BAROMETERS.

=19. The Common Form.=--The barometer is of great use to the mariner, who,
by using it as a "weather glass," is enabled to foresee and prepare for
sudden changes in the weather. For marine purposes, the lower portion of
the glass tube of the barometer must be contracted to a fine bore, to
prevent oscillation in the mercurial column, which would otherwise be
occasioned by the movements of the ship. This tube is cemented to the
cistern, which is made of boxwood, and has a moveable leathern bottom, for
the purpose of rendering the instrument portable, by screwing up the
mercury compactly in the tube. The tube is enclosed in a mahogany frame,
which admits of a variety of style in shape, finish, and display, to meet
the different fancies and means of purchasers. The frame is generally
enlarged at the upper part to receive the scales and the attached
thermometer, which are covered by plate glass. The cistern is encased in
brass for protection, the bottom portion unscrewing to give access to the
portable screw beneath the cistern. Figs. 13 and 14 illustrate this form
of barometer. Marine barometers require to be suspended, so that they may
remain in a vertical position under the changeable positions of a vessel
at sea. To effect this they are suspended in gimbals by a brass arm. The
gimbals consist of a loose ring fastened by thumb-screws to the middle
part of the frame of the barometer, in front and back. The forked end of
the arm supports this ring at the sides, also by the aid of thumb-screws.
Hence the superior weight of the cistern end is always sufficient to cause
the instrument to move on its bearing screws, so as always to maintain a
perpendicular position; in fact, it is so delicately held that it yields
to the slightest disturbance in any direction. The other end of the arm is
attached to a stout plate, having holes for screws, or fitted to slip into
a staple or bracket, by which it may be fixed to any part of the cabin of
a ship; the arm is hinged to the plate, for the purpose of turning the arm
and barometer up whenever it is desirable.

[Illustration: Fig. 13.]

[Illustration: Fig. 14.]

Other forms of barometer (to be immediately described) have superseded
this in the British Marine, but the French still give the preference to
the wooden frames. They think the barometer can be more securely mounted
in wood, is more portable, and less liable to be broken by a sudden
concussion than if fitted in a metal frame. The English deem the ordinary
wooden barometers not sufficiently accurate, owing to the irregular
expansion of wood, arising from its hygrometric properties. Some of the
English opticians have shown that very portable, and really accurate
barometers can be made in brass frames, and therefore the preference is
now given to this latter material.


=20. The Kew Marine Barometer.=--The form of barometer so-called, is that
recommended by the Congress of Brussels, held in 1853, for the purpose of
devising a systematic plan of promoting meteorological observations at
sea.

The materials employed in its construction are mercury, glass, iron, and
brass. The upper part of the tube is carefully calibrated to ensure
uniformity of bore, as this is a point upon which the accuracy of the
instrument to some extent depends. At sea, the barometer has never been
known to stand above 31 inches, nor below 27. These extremes have been
attained with instruments of undoubted accuracy, but they are quite
exceptional. It is not necessary, therefore, to carry the scales of marine
barometers beyond these limits, but they should not be made shorter. If
the vernier is adjusted to read upward, the scale should extend to 32
inches, to allow room for the vernier to be set to 31 inches at least.
Cases have occurred in which this could not be done, and rare, but
valuable observations have been lost in consequence. If the scale part of
the tube be not uniform in bore, the index error will be irregular
throughout the scale. Whether the bore of the rest of the tube varies in
diameter, is of no moment. From two to three inches below the measured
part, the bore is contracted very much, to prevent the pulsations in the
mercurial column--called "pumping"--which, otherwise, would occur at sea
from the motion of the ship. In ordinary marine barometers, this
contraction extends to the end of the tube. Below the contracted part is
inserted a pipette--or Gay Lussac air-trap--which is a little elongated
funnel with the point downwards. Its object is to arrest any air that may
work in between the glass and the mercury. The bubble of air lodges at the
shoulder, and can go up no farther. It is one of those simple contrivances
which turn out remarkably useful. If any air gets into the tube, it does
not get to the top, and therefore does not vitiate the performance of the
barometer; for the mercury itself works up and down through the funnel.
Below this, the tube should not be unnecessarily contracted.

[Illustration: Fig. 15.]

The open end of the tube is fixed into an iron cylinder, which forms the
cistern of the barometer. Iron has no action upon mercury, and is
therefore used instead of any other metal. One or two holes are made in
the top of the cistern, which are covered on the inside with strong
sheep-skin leather, so as to be impervious to mercury, but sufficiently
porous for the outer air to act upon the column. The cistern is of
capacity sufficient to receive the mercury which falls out of the tube
until the column stands lower than the scale reads; and when the tube is
completely full, there is enough mercury to cover the extremity so as to
prevent access of air. There is no screw required for screwing up the
mercury.

The glass tube thus secured to the cistern is protected by a brass tubular
frame, into which the iron cistern fits and screws compactly. Cork is used
to form bearings for the tube. A few inches above the cistern is placed
the attached thermometer. Its bulb is enclosed in the frame, so as to be
equally affected by heat with the barometric column. The upper end of the
frame is fitted with a cap which screws on, and embraces a glass shield
which rests in a gallery formed on the frame below the scale, and serves
to protect the silvered scale, as well as the inner tube, from dust and
damp. A ring, moveable in a collar fixed on the frame above the centre of
gravity of the instrument, is attached to gimbals, and the whole is
supported by a brass arm in the usual manner; so that the instrument can
be moved round its axis to bring any source of light upon it, and will
remain vertical in all positions of the ship. The vernier reads to
five-hundredths of an inch. No words are placed upon the scale, as the old
formulary was deemed misleading. The vernier can be set with great
exactness, as light is admitted to the top of the mercury by a front and
a back slit in the frame. The lower edge of the vernier should be brought
to the top of the mercury, so as just to shut out the light.

It is evident that this form of barometer must be more reliable in its
indications than those in wooden frames. The graduations can be accurately
made, and they will be affected only by well-known alterations due to
temperature. Some think the tube is too firmly held, and therefore liable
to be broken by concussion more readily than that of an inferior
instrument. This, however, appears a necessary consequence of greater
exactness. It is an exceedingly good portable instrument, and can be put
up and taken down very readily. These barometers are preferred to marine
barometers in wood, wherever they have been used. In merchant ships, and
under careful treatment, they have been found very durable. They may be
sent with safety by railway, packed carefully in a wooden box.

_Directions for Packing._--In removing this barometer it is necessary to
slope it gradually till the mercury reaches the top of the tube. It is
then portable, if carried cistern end upwards or lying flat. If carried
otherwise, it will very probably be broken by the jerking motion of the
heavy mercury in the glass tube. Of course it must not be jarred, or
receive concussion.

_Position for Marine Barometer._--Admiral FitzRoy, to whose valuable
papers we are much indebted, writes in his "Barometer Manual":--"It is
desirable to place the barometer in such a position as not to be in danger
of a side blow, and also sufficiently far from the deck above to allow for
the spring of the metal arm in cases of sudden movements of the ship.

"If there is risk of the instrument striking anywhere when the vessel is
much heeled, it will be desirable to put some soft padding on that place,
or to check movement in that direction by a light elastic cord; in fixing
which, attention must be paid to have it acting only where risk of a blow
begins, not interfering otherwise with the free swing of the instrument: a
very light cord attached above, when possible, will be least likely to
interfere injuriously."


=21. Method of verifying Marine and other Barometers.=--"In nearly all the
barometers which had been employed at sea till recently the index
correction varied through the range of scale readings, in proportion to
the difference of capacity between the cistern and the tube. To find the
index correction for a land barometer, comparison with a standard, at any
part of the scale at which the mercury may happen to be, is generally
considered sufficient. To test the marine barometer is a work of much more
time, since it is necessary to find the correction for scale readings at
about each half inch throughout the range of atmospheric pressure to which
it may be exposed; and it becomes necessary to have recourse to artificial
means of changing the pressure of the atmosphere on the surface of the
mercury in the cistern.

"The barometers to be thus tested are placed, together with a standard, in
an air-tight chamber, to which an air-pump is applied, so that, by
partially exhausting the air, the standard can be made to read much lower
than the lowest pressure to which marine barometers are likely to be
exposed; and by compressing the air it can be made to read higher than the
mercury ever stands at the level of the sea. The tube of the standard is
contracted similarly to that of the marine barometer, but a provision is
made for adjusting the mercury in its cistern to the zero point. Glass
windows are inserted in the upper part of the iron air-chamber, through
which the scales of the barometers may be seen; but as the verniers cannot
be moved in the usual way from outside the chamber, a provision is made
for reading the height of the mercury independent of the verniers attached
to the scales of the respective barometers. At a distance of some five or
six feet from the air-tight chamber a vertical scale is fixed. The
divisions on this scale correspond exactly with those on the tube of the
standard barometer. A vernier and telescope are made to slide on the scale
by means of a rack and pinion. The telescope has two horizontal wires, one
fixed and the other moveable by a micrometer screw, so that the difference
between the height of the column of mercury and the nearest division on
the scale of the standard, and also of all the other barometers placed by
the side of it for comparison, can be measured either with the vertical
scale and vernier or the micrometer wire. The means are thus possessed of
testing barometers for index error in any part of the scale, through the
whole range of atmospheric pressure to which they are likely to be
exposed; and the usual practice is to test them at every half inch from
27.5 to 31 inches.

"In this way barometers of various other descriptions have been tested,
and some errors found to be so large that a few barometers read half an
inch and upwards too high, while others read as much too low. In some
cases those which were correct in one part of the scale were found to be
from half an inch to an inch wrong in other parts. These barometers were
of an old and ordinary, not to say inferior, construction. In some the
mercury would not descend lower than about 29 inches, owing to a fault
very general in the construction of many common barometers till lately in
frequent use:--the _cistern was not large enough_ to hold the mercury
which descended from the tube in a _low atmospheric pressure_.

"When used on shore, this contraction of the tube causes the marine
barometer to be _sometimes_ a little behind an ordinary land barometer,
the tube of which is not contracted. The amount varies according to the
rate at which the mercury is rising or falling, and ranges from 0.00 to
0.02 of an inch. As the motion of the ship at sea causes the mercury to
pass more rapidly through the contracted tube, the readings are almost the
same there as they would be if the tube were not contracted, and in no
case do they differ enough to be of importance in maritime use."

The cistern of this marine barometer is generally made an inch and a
quarter in diameter, and the scale part of the tube a quarter of an inch
in bore. The inches on the scale, instead of being true, are shortened by
.04 of an inch, in order to avoid the necessity of applying a correction
due to the difference of capacity of the tube and cistern. This is done
with much perfection, and the errors of the instruments, when compared
with a standard by the apparatus used at Kew and Liverpool Observatories,
are determined to the thousandth of an inch, and are invariably very
uniform and small. The error so determined includes the correction due to
capillarity, capacity, and error of graduation, and forms a constant
correction, so that only one variable correction, that due to temperature,
need be applied, when the barometer is suspended near the water line of
the ship, to make the observations comparable with others. With all the
advantages of this barometer, however, it has recently been superseded, to
some extent, because it was found to require more care than could
ordinarily be expected to be given to it by the commander of a ship.
Seamen do not exactly understand the value of such nice accuracy as the
thousandth part of an inch, but prefer an instrument that reads only to a
hundredth part.


22. THE FITZROY MARINE BAROMETER.

Admiral FitzRoy deemed it desirable to construct a form of barometer as
practically useful as possible for marine purposes. One that should be
less delicate in structure than the Kew barometer, and not so finely
graduated. One that could be set at a glance and read easily; that would
be more likely to bear the common shocks unavoidable in a ship of war.
Accordingly, the Admiral has devised a barometer, which he has thus
described:--

"This marine barometer, for Her Majesty's service, is adapted to _general_
purposes.

"It differs from barometers hitherto made in points of detail, rather than
principle:--1. The glass tube is packed with vulcanised india-rubber,
which checks vibration from concussion; but does not hold it rigidly, or
prevent expansion. 2. It does not oscillate (or pump), though extremely
sensitive. 3. The scale is porcelain, _very legible_, and not liable to
change. 4. There is no iron anywhere (_to rust_). 5. Every part can be
unscrewed, examined, or cleaned, by any careful person. 6. There is a
_spare_ tube, fixed in a cistern, filled with boiled mercury, and _marked_
for adjustment in this, or _any similar_ instrument.

"These barometers are graduated to hundredths, and they will be found
accurate to _that_ degree, namely the second decimal of an inch.

"They are packed with vulcanised caoutchouc, in order that (by this, and
by a peculiar strength of glass tube) guns may be fired near these
instruments without causing injury to them by ordinary concussion.

"It is hoped that all such instruments, for the public service at sea,
will be quite similar, so that any spare tube will fit _any_ barometer.

"_To Shift a Tube._--Incline the barometer slowly, and then take it down,
after allowing the mercury to fill the upper part. Lay the instrument on a
table, unscrew the outer cap at the joining just below the cistern swell,
then unscrew the tube _and_ cistern, by turning the cistern gently,
against the sun, or to _the left_, and draw out the tube very carefully
_without bending it in the least_, _turning_ it a little, if required, as
moved. Then insert the new tube very cautiously, screw in, and adjust to
the diamond-cut mark for 27 inches. Attach the cap, and suspend the
barometer for use.

"If the mercury does not immediately quit the top of the tube, tap the
cistern end rather sharply. In a well-boiled tube, with a good vacuum, the
mercury hangs, at times, so adhesively as to deceive, by causing a
supposition of some defect.

"In about ten minutes the mercurial column should be nearly right; but as
local temperature affects the brass, as well as the mercury, slowly and
unequally, it may be well to defer any _exact comparisons with other
instruments_ for some few hours."

Messrs. Negretti and Zambra are the makers of these barometers for the
Royal Navy. Fig. 16 is an illustration.

[Illustration: Fig. 16.]

The tube is fixed to a boxwood cistern, which is plugged with very porous
cane at the top, to allow of the ready influence of a variation in
atmospheric pressure upon the mercury. Round the neck of the cistern is
formed a brass ring, with a screw thread on its circumference. This screws
into the frame, and a mark on the tube is to be adjusted to 27 inches on
the scale, the cistern covering screwed on, and the instrument is ready to
suspend. The frame and all the fittings are brass, without any iron
whatever; because the contact of the two metals produces a galvanic
action, which is objectionable. The spare tube is fitted with
india-rubber, and ready at any time to replace the one in the frame. The
ease with which a tube can be replaced when broken is an excellent feature
of the instrument. The spare tube is carefully stowed in a box, which can
also receive the complete instrument when not in use. All the parts are
made to a definite gauge; the frames are, therefore, all as nearly as
possible similar to each other, and the tubes--like rifle bullets--are
adjustible to any frame. If, then, the tube in use gets broken, the
captain can replace it by the other; but, as it is securely packed with
india-rubber, there is very little liability of its being broken by fair
usage. Every person who knows the importance of the barometer on board
ship, will acknowledge that the supplementary tube is a decided
improvement. Many instruments of this description are afloat in the Royal
Navy, and in a short time it may be expected that all the frames and tubes
of barometers in the public service at sea will be similar in size and
character; so that should a captain have the misfortune to get both his
tubes broken, he would be able to borrow another from any ship he fell in
with that had one to spare, which would be perfectly accurate, because it
would have been verified before it was sent out.


=23. Admiral FitzRoy's Words for the Scale.=--The graduation of inches and
decimals are placed in this barometer on the right-hand side of the tube;
and on a similar piece of porcelain, on the left-hand, are engraved, as
legibly as they are expressed succinctly, the following words, of
universal application in the interpretation of the barometer movements:--

     _RISE_            _FALL_
      FOR               FOR
      COLD              WARM
      DRY               WET
       OR                OR
      LESS              MORE
      WIND.             WIND.
    --------          --------
     EXCEPT            EXCEPT
    WET FROM          WET FROM
   COOLER SIDE.      COOLER SIDE.

Reverting to the explanation of the words on the "Coast" barometers (at
page 14), and comparing and considering them as given for northern
latitudes, and as they must be altered for southern latitudes, it will be
perceived, that for all _cold_ winds the barometer rises; and falls for
_warm_ winds. The mercury also falls for _increased_ strength of wind; and
rises as the wind _lulls_. Likewise before or with rain the column of
mercury falls; but it rises with fine dry weather. Putting these facts
together, and substituting for the points of the compass the terms "cold"
and "warm," the appropriateness of the words on the scale of this
barometer is readily perceived. These concise and practical indications of
the movements in the barometer are applicable for instruments intended for
use in any region of the world, and are in perfect accordance with the
laws of winds and weather deduced by Dove and other meteorologists. There
is nothing objectionable in them, and being founded upon experience and
the deductions made from numerous recorded observations of the weather in
all parts of the world, as well as confirmed by the theories of science,
they may consequently be considered as generally reliable. They involve no
conjecture, but express succinctly scientific principles.


=24. Trials of the FitzRoy Marine Barometer under Fire of Guns.=--Some of
the first barometers made by Messrs. Negretti and Zambra on Admiral
FitzRoy's principle were severely tried under the heaviest naval gun
firing, on board H.M.S. _Excellent_; and under all the circumstances, they
withstood the concussion. The purpose of the trials was "to ascertain
whether the _vulcanized india-rubber packing_ round the glass tube of a
_new marine barometer_ did check the vibration caused by firing, and
whether guns might be fired close to these instruments without causing
injury to them." In the first and second series of experiments, a marine
barometer on Admiral FitzRoy's plan was tried against a marine barometer
on the Kew principle, both instruments being new, and treated in all
respects similarly. They were "hung over the gun, under the gun, and by
the side of the gun, the latter both inside and outside a bulkhead,--in
fact, in all ways that they would be tried in action with the bulkheads
cleared away." The result was that the Kew barometer was broken and
rendered useless, while the new pattern barometer was not injured in the
least. In a third series of experiments, Mr. Negretti being present, five
of the new pattern barometers were subjected to the concussion produced by
firing a 68-pounder gun with shot, and 16 lbs. charge of powder. They were
suspended from a beam immediately under the gun, then from a beam
immediately over the gun, and finally they were suspended by the arm to a
bulkhead, at a distance of only 3 ft. 6 in. from the axis of the gun; and
the result was, according to the official report, "that all these
barometers, however suspended, would stand, without the slightest injury,
the most severe concussion that they would ever be likely to experience in
any sea-going man-of-war." These trials were conducted under the
superintendence of Captain Hewlett, C.B., and the guns were fired in the
course of his _usual_ instructions. His reports to Admiral FitzRoy, giving
all the particulars of the trials, are published in the "Ninth Number of
Meteorological Papers," issued by the Board of Trade.[2]


25. NEGRETTI AND ZAMBRA'S FARMER'S BAROMETER AND DOMESTIC WEATHER-GLASS.

It is a well-known fact that the barometer is as much, or even more
affected by a change of wind as it is by rain; and the objection raised
against a simple barometer reading, as leaving the observer in doubt
whether to expect wind or rain, is removed by the addition of the
Hygrometer, an instrument indicating the comparative degree of dryness or
dampness of the air;--a most important item in the determination of the
coming weather.

The farmer should not be content to let his crops lie at the mercy, so to
speak, of the weather, when he has within his command instruments which
may be the means of preventing damage to, and in cases total loss of, his
crops.

The farmer hitherto has had to depend for his prognostication of the
weather on his own unassisted "Weather Wisdom;" and it is perfectly
marvellous how expert he has become in its use. Science now steps in, not
to ignore this experience, but on the contrary, to give it most valuable
assistance by extending it, and enabling it to predict, with an accuracy
hitherto unknown, the various changes that take place in this most
variable of climates.

To the invalid, the importance of predicting with tolerable accuracy the
changes that are likely to occur in the weather, cannot be over-rated.
Many colds would be prevented, if we could know that the morning so balmy
and bright, would subside into a cold and cheerless afternoon. Even to the
robust, much inconvenience may be prevented by a due respect to the
indications of the hygrometer and the barometer, and the delicate in
health will do well to regard its warnings.

[Illustration: Fig. 17.]

_Description of the Instrument._--The farmer's barometer, as figured in
the margin, consists of an upright tube of mercury inverted in a cistern
of the same fluid; this is secured against a strong frame of wood, at the
upper end of which is fixed the scale, divided into inches and tenths of
an inch. On either side of the barometer, or centre tube, are two
thermometers--that on the left hand has its bulb uncovered and freely
exposed, and indicates the temperature of the air at the place of
observation; that on the right hand has its bulb covered with a piece of
muslin, from which depend a few threads of soft lamp cotton; this cotton
is immersed in the small cup situated just under the thermometer, this
vessel being full of water; the water rises by capillary attraction to the
muslin-covered bulb, and keeps it in a constantly moist state.

These two thermometers, which we distinguish by the names "Wet Bulb" and
"Dry Bulb," form the Hygrometer; and it is by the simultaneous reading of
these two thermometers, and noting the difference that exists between
their indications, that the humidity in the atmosphere is determined.

Admiral FitzRoy's words (see p. 22) are placed upon the scale of the
barometer, as the value of a reading depends, not so much on the actual
height of the mercury in the tube, as it does on whether the column is
rising, steady, or falling.

The moveable screw at the bottom of the cistern is for the purpose of
forcing the mercury to the top of the tube when the instrument is being
carried from place to place, and it must always be unscrewed to its utmost
limit when the barometer is hung in its proper place. After this it should
never be touched.

The manner in which the Hygrometer acts is as follows: It is a pretty
well-known fact that water or wine is often cooled by a wet cloth being
tied round the bottle, and then being placed in a current of air. The
evaporation that takes place in the progressive drying of the cloth causes
the temperature to fall considerably below that of the surrounding
atmosphere, and the contents of the bottle are thus cooled. In the same
manner, then, the covered wet bulb thermometer will be found _invariably_
to read lower than the uncovered one; and the greater the dryness of the
air, the greater will be the difference between the indications of the
two thermometers; and the more moisture that exists in the air, the more
nearly they will read alike.

The cup must be kept filled with pure water, and occasionally cleaned out,
to remove any dirt. The muslin, or cotton-wick, should also be renewed
every few weeks. The hygrometer may be had separate from the barometer, if
the combined instruments cannot be sufficiently exposed to the external
air, this being essential for the successful use of the hygrometer.

This farmer's weather-glass, then, consists of three distinct instruments:
the barometer, the thermometer, and the hygrometer. He has thus at command
the three instrumental data necessary for the prediction of the weather.
And now to describe--

_How to Use the Instrument._--The observations should be taken twice a
day, say at 9 A.M. and 3 P.M.; and should be entered on a slip of paper,
or a slate hung up by the barometer. The observer will then be able to see
the different values of the readings from time to time, and to draw his
conclusions therefrom.

The thermometer on the left hand should first be read, and a note made of
its indication, which is the temperature of the air. The wet bulb
thermometer should now be read, and also noted; and the difference should
be taken of these two readings. Next read the barometer by moving the
small index at the side of the tube until it is on a level with the top of
the mercury. Having noted the number of inches at which the column stands,
compare with the last observation, and see immediately whether the
barometer is rising, steady, or falling.

Now, having taken the observations as above, we naturally ask the
question, _What are we to predict from them?_

And, probably, the best way of answering this query will be by giving an
example. We will suppose that our readings yesterday were as
follows:--Temperature, 70 deg.; Wet Bulb, 69 deg.; Difference, 1 deg.; =very moist
air. Barometer, 29.5, and that rain has fallen.

To-day, we read:--Temperature, 60 deg.; Wet Bulb, 55 deg.; Difference, 5 deg.; =dryer
air. Barometer, 30. We may safely predict that the rain will cease, and
probably we may have wind from the northward.

In spring or autumn, if the barometric height be steady any where between
29.5 and 30 inches, with the temperature about 60 deg., fresh to moderate
south-westerly winds, with cloudy sky, will probably characterize the
weather; the indications of the hygrometer being then specially
serviceable in enabling us to foretell rain; but if the mercury become
steady at about 30.5 inches, with temperature about 40 deg., north-easterly
winds, dry air, and clear sky, may be confidently expected.

Many cases will doubtless suggest themselves to the observer where these
figures do not occur, and where he might find a difficulty in interpreting
the indications of his instruments. We have, therefore, drawn up some
concise rules for his guidance; and although they will not prove
absolutely infallible guides to this acknowledged most difficult problem,
still, they will be found of much service in foretelling the weather, when
added to an intelligent observation of ordinary atmospheric phenomena, as
force and direction of wind, nature of any particular season, and the time
of year.


26. RULES FOR FORETELLING THE WEATHER.

A RISING BAROMETER.

    A "Rapid" rise indicates unsettled weather.

    A "Gradual" rise indicates settled weather.

    A "Rise," with dry air, and cold increasing in summer, indicates wind
    from northward; and if rain has fallen, better weather is to be
    expected.

    A "Rise," with moist air and a low temperature, indicates wind and
    rain from northward.

    A "Rise," with southerly wind, indicates fine weather.

A STEADY BAROMETER,

    With dry air and a seasonable temperature, indicates a continuance of
    very fine weather.

A FALLING BAROMETER.

    A "Rapid" fall indicates stormy weather.

    A "Rapid" fall, with westerly wind, indicates stormy weather from
    northward.

    A "Fall," with a northerly wind, indicates storm, with rain and hail
    in summer, and snow in winter.

    A "Fall," with increased moisture in the air, and the heat increasing,
    indicates wind and rain from southward.

    A "Fall," with dry air, and cold increasing (in winter), indicates
    snow.

    A "Fall," after very calm and warm weather, indicates rain with
    squally weather.


=27. Causes which may bring about a Fall or a Rise in the
Barometer.=[3]--As heat produces rarefaction, a sudden rise of temperature
in a distant quarter may affect the weight of the atmosphere over our
heads, by producing an aerial current outwards, to supply the place of the
lighter air which has moved from its former position; in which case the
barometer will fall. Now such a movement in the atmosphere is likely to
bring about an intermixture of currents of air of different temperatures,
and from this intermixture rain is likely to result.

On the other hand, as cold produces condensation, any sudden fall of
temperature causes the column of air over the locality to contract and
sink to a lower level, whilst other air rushes in from above to supply the
void; and, accordingly, the barometer rises. Should this air, as often
happens, proceed from the north, it will contain in general but little
moisture; and hence, on reaching a warmer latitude, will take up the
vapour of the air, so that dry weather will result.

It is generally observed, that wind causes a fall in the instrument; and,
indeed, in those greater movements of the atmosphere which we denominate
storms or hurricanes, the depression is so considerable as to forewarn
the navigator of his impending danger. It is evident, that a draught of
air in any direction must diminish the weight of the column overhead, and
consequently cause the mercury in the barometer to sink.

The connection, therefore, of a sinking of the barometric column with rain
is frequently owing to the wind causing an intermixture of the aerial
currents which, by their motion, diminish the weight of the atmosphere
over our heads; whilst a steady rise in the column indicates the absence
of any great atmospheric changes in the neighbourhood, and a general
exemption from those causes which are apt to bring about a precipitation
of vapour.


=28. Use of the Barometer in the management of Mines.=--The inflammable
and suffocating gases, known to coal-miners as fire-damp and choke-damp,
are specifically heavier than air; and as they issue from the fissures of
the mine, or are released from the coal, the atmospheric pressure tends to
drive them into the lowest and least ventilated galleries. Consequently a
greatly reduced atmospheric pressure will favour a sudden outflow or
advance of gas; whence may result cases of explosion or suffocation. It
has been found that these accidents occur for the most part about the time
of a low barometric column. A reliable barometer should, therefore, be
systematically consulted by those entrusted with the management or control
of coal-mines, so that greater vigilance and caution may be enjoined on
the miners whenever the mercury falls low, especially after it has been
unusually high for some days.


=29. Use of the Barometer in estimating the Height of Tides.=--The
pressure of the atmosphere affects the height of the tide, the water being
in general higher as the barometer is lower. The expressions of seamen,
that "frost nips the tide," and "fog nips the tide," are explained by the
high barometer which usually accompanies frost and fog. M. Daussy, Sir J.
C. Ross, and others, have established that a rise of one inch in the
barometer will have a corresponding fall in the tide of about one foot.
Therefore navigators and pilots will appreciate the following suggestion
of Admiral FitzRoy:--

"Vessels sometimes enter docks, or even harbours, where they have scarcely
a foot of water more than their draught; and as docking, as well as
launching large ships, requires a close calculation of height of water,
the state of the barometer becomes of additional importance on such
occasions."




CHAPTER II.

SYPHON TUBE BAROMETERS.


=30. Principle of.=--If some mercury, or any other fluid, be poured into a
tube of glass, bent in the form of =U=, and open at both ends, it will
rise to the same height in both limbs, the tube being held vertically. If
mercury be poured in first, and then water upon it at one end, these
liquids will not come to the same level; the water will stand much higher
than the mercury. If the height of the mercury, above the line of meeting
of the fluids, be one inch, that of the water will be about
thirteen-and-a-half inches. The explanation of this is, that the two
columns balance each other. The pressure of the atmosphere in each limb is
precisely similar; but the one column stands so much higher than the
other, because the fluid of which it is composed is so much lighter, bulk
for bulk, than the other. If one end of the tube be hermetically closed,
the other limb be cut off within a few inches of the bend, and the tube
carefully filled with mercury; by placing it in a vertical position, the
mercury will fall, if the closed limb be long enough, until it is about
thirty inches higher than that in the exposed limb, where it will remain.
Here the atmosphere presses upon the short column; but not upon the long
one. It is this pressure, therefore, which maintains the difference of
level. In fact, it forms a barometer without a cistern, the short limb
answering the purpose of a cistern. The first barometers on this principle
were devised by the celebrated philosopher, Dr. Hook, as described in the
next section.


31. DIAL, OR WHEEL BAROMETERS.

The familiar household "Weather Glasses" are barometers on the syphon
principle. The portions of the two limbs through which the mercury will
rise and fall with the varying pressure of the atmosphere are made of
precisely the same diameter; while the part between them is contracted. On
the mercury, in the exposed limb, rests a round float of ivory or glass;
to this a string is attached and passed over and around a brass pulley,
the other end carrying another lighter weight. The weight resting on the
mercury rises and falls with it. On the spindle of the pulley, which
passes through the frame and centre of the dial-plate, is fixed a light
steel hand, which revolves as the pulley turns round. When the mercury
falls for a decrease of atmospheric pressure, it rises by the same
quantity in the short tube, and pushes up the float, the counterpoise
falls, and thus moves the hand or pointer to the left. When the pressure
increases, the pointer is drawn in a similar manner to the right.

[Illustration: Fig. 18.]

[Illustration: Fig. 19.]

[Illustration: Fig. 20.]

The dials are generally made of metal silvered over or enamelled, but
porcelain may be used. If the circumference of the pulley, or "wheel," be
two inches, it will revolve once for an alteration of level amounting to
two inches in each tube, or four inches in the height of the barometric
column; and as the dial may be from twenty to thirty-six inches in
circumference, five to nine inches on the graduated scale corresponds to
one inch of the column; and hence the sub-divisions are distinctly
perceptible, and a vernier is not necessary.

The motion of the pointer alone is visible; and a mahogany, or rosewood,
frame, supports, covers, and renders the instrument ornamental and
portable. In the back of the frame is a hinged door, which covers the
cavity containing the tube and fixtures. The dial is covered by a glass in
a brass rim, similar to a clock face. A brass index, working over the
dial, moveable by a key or button, may be applied, and will serve to
register the position of the hand when last observed. These instruments
are usually fitted with a thermometer, and a spirit level; the latter for
the purpose of getting the instrument perfectly vertical. They sometimes
have, in addition, a hygrometer, a sympiesometer, an aneroid, a mirror, or
a clock, &c., singly or combined. The frame admits of much variety of
style and decoration. It may be carved or inlaid. The usual adjustment of
scale is suited for localities at no considerable elevation above the
sea. Accordingly, being commercial articles, they have been found
frequently quite out of place. When intended for use at high elevations,
they should have a special adjustment of scale. As household instruments
they are serviceable, and ornamental. But the supply-and-demand principle
upon which they are sold, has entailed upon those issued by inferior
makers a generally bad adjustment of scale. The illustrations are those of
ordinary designs.

[Illustration: Fig. 21.]

[Illustration: Fig. 22.]

[Illustration: Fig. 23.]

Dial barometers required for transmission to distant parts, as India and
the Colonies, are furnished with a steel stop-cock, to render them
portable more effectually than can be done by the method of _plugging_ the
tube.


32. STANDARD SYPHON BAROMETER.

Fig. 24 represents the most accurate form of the Gay Lussac barometer. The
short limb is closed at the top, after the mercury is introduced, and a
small lateral puncture is made at _a_, which is covered over with a
substance which permits the access of air, but prevents the escape of any
mercury when the instrument is packed for travelling. The bent part of the
tube is contracted to a capillary bore; and just above this, in the long
limb, is placed the air-trap, already described (see p. 17), and here
illustrated (fig. 25). When reversed, as it must be for portability, the
capillary attraction keeps the mercury in the long branch. Should the
mercury of the short column get detached, some small quantity of air _may_
pass; but it will be arrested at the pipette, and will not vitiate the
length of the barometric column. It can be easily expelled by gently
shaking or tapping the instrument before suspending it for observation. In
the illustration, the zero of the scale is placed at Z, near the middle of
the tube; and the graduations extend above and below. In making an
observation, it is necessary to take the reading ZA on the long branch,
and ZB on the short one. The sum of the two gives the height of the
barometer. The zero of the scale in some instruments is placed low down,
so as to require the difference of the two readings to be taken. A
thermometer is attached to the frame as usual.

[Illustration: Fig. 24.]

[Illustration: Fig. 25.]

These instruments can be very accurately graduated, and are very exact in
their indications, provided great care has been exercised in selecting the
tubes, which must be of the same calibre throughout the parts destined to
measure the variations of atmospheric pressure. They should be suspended
so as to insure their hanging vertically.

The syphon barometer does not require correction for capillarity nor for
capacity, as each surface of the mercury is equally depressed by capillary
attraction, and the quantity of mercury which falls from the long limb of
the tube occupies the same length in the short one. The barometric height
must, however, be corrected for temperature, as in the cistern barometer.
Tables containing the temperature corrections to be applied to barometer
readings for scales engraved on the glass tube, or on brass or wood
frames, are published.




CHAPTER III.

BAROGRAPHS, OR SELF-REGISTERING BAROMETERS.


=33. Milne's Self-Registering Barometer.=--For a long time a good and
accurate self-recording barometer was much desired. This want is now
satisfactorily supplied, not by one, but by several descriptions of
apparatus. The one first to be described was the design of Admiral Sir A.
Milne, who himself constructed, in 1857, we believe, the original
instrument, which he used with much success. Since that time several of
these instruments have been made, and have performed satisfactorily. The
barometer tube is a syphon of large calibre, provided with a Gay Lussac
pipette, or air-trap; and fitted with a float, a wheel, and a pointer, as
in the "Dial" barometer. The float is attached to a delicate watch-chain,
which passes over the wheel and is adequately counterpoised. Behind the
indicating extremity of the pointer or hand is a projecting point, which
faces the frame of the instrument, and is just within contact with the
registering paper. A clock is applied, and fitted with auxiliary
mechanism, so as to be able to move the mounted paper with regularity
behind the pointer, and at designed equal intervals of time to release a
system of levers and springs, so as to cause the marker to impress a dot
on the paper, either by puncture or pencil-mark. The paper is ruled with
horizontal lines for the range of the mercurial column, and parallel arcs
of circles for the hours. Thus the barometer is rendered self-recording,
by night or day, for a week or more; hence the great value of the
instrument. The clock, index, and registering mechanism are protected from
dust and interference by a glass front, hinged on and locked. As the
temperature of the mercury is not registered, there is fixed to the frame
a Sixe's thermometer to record the maximum and minimum temperatures, which
should be noted at least every twenty-four hours.

Admiral FitzRoy has suggested the name "Atmoscope" for Admiral Milne's
barometer; and he has also termed it a "Barograph." This latter word
appears to be applicable to all kinds of self-registering barometers
hitherto designed. Of the arrangement under consideration Admiral FitzRoy
writes:--"It shows the alterations in tension, or the pulsations, so to
speak, of atmosphere, on a large scale, by hourly marks; and the diagram
expresses, to a practised observer, what the 'indicator card' of a
steam-cylinder shows to a skilful engineer, or a stethescope to a
physician."


[Illustration: Fig. 26.]

=34. Modification of Milne's Barometer.=--The great difficulty to be
overcome in Milne's barometer, is to adjust the mechanism for obtaining
registration so that the action of the striker upon the pointer should not
in the slightest degree move it from its true position. A different mode
of registration, capable of recording accurately the least appreciable
movement of the mercurial column, has been effected. In this instrument
the registering paper is carried upon a cylinder or drum. By reference to
the illustration, Fig. 26, the details of construction will be readily
understood. It should, however, be mentioned, that it is not a picture of
the outward appearance of the instrument. The position of the barometer
should be behind the clock; it is represented on one side merely for the
purpose of clearly illustrating the arrangement and principles. The
instrument has a large syphon barometer tube, in which the mercurial
column is represented. On the mercury at _A_, in its open end, rests a
glass float, attached to a watch-chain, or suitable silken cord, the other
end of which is connected to the top of the arched head on the short arm
of a lever-beam. The long arm of the beam is twice the length of the short
arm, for the following reason. As the mercury falls in the long limb, it
rises through an equal space in the short limb of the tube, and _vice
versa_. But the barometric column is the difference of height of the
mercury in the two limbs; hence the rise or fall of the float through
half-an-inch will correspond to a decrease or an increase of the
barometric column of one inch. In order, then, to record the movements of
the barometric column, and not those of the float, the arm of the beam
connected with the float is only half the radius of the other arm. Both
arms of the beam carry circular-arched heads, which are similar portions
of the complete circles, the centre of curvature being the fulcrum, or
axis. This contrivance maintains the leverage on each extremity of the
beam always at the same distance from the fulcrum. From the top of the
large arched head a piece of watch-chain descends, and is attached to the
marker, _B_, which properly counterpoises the float, _A_, and is capable
of easy movement along a groove in a brass bar, so as to indicate the
barometric height on an ivory scale, _C_, fixed on the same vertical
framing. On the opposite side of the marker, _B_, is formed a metallic
point, which faces the registration sheet and is nearly in contact with
it. The framing, which carries the scale and marker, is an arrangement of
brass bars, delicately adjusted and controlled by springs, so as to permit
of a quick horizontal motion, in a small arc, being communicated to it by
the action of the hammer, _E_, of the clock, whereby the point of the
marker is caused to impress a dot upon the paper. The same clock gives
rotation to the hollow wooden cylinder, _D_, upon which is mounted the
registering paper. The clock must be rewound when a fresh paper is
attached to the cylinder, which may be daily, weekly, or monthly,
according to construction; and the series of dots impressed upon the paper
shows the height of the barometric column every hour by day and night. The
space traversed by the marker is precisely equal to the range of the
barometric column.


=35. King's Self-Registering Barometer.=--Mr. Alfred King, Engineer of the
Liverpool Gas-light Company, designed, so long ago as 1854, a barometer to
register, by a continuous pencil-tracing, the variations in the weight of
the atmosphere; and a highly-satisfactory self-recording barometer, on his
principle and constructed under his immediate superintendence, has quite
recently been erected at the Liverpool Observatory.

[Illustration: Fig. 27.]

Fig. 27 is the front elevation of this instrument. _A_, the barometer
tube, is three inches in internal diameter, and it floats freely (not
being fixed as usual) in the fixed cistern, _B_, guided by
friction-wheels, _W_. The top end of the tube is fastened to a peculiar
chain, which passes over a grooved wheel turning on finely-adjusted
friction rollers. The other end of the chain supports the frame, _D_,
which carries the tracing pencil. The frame is suitably weighted and
guided, and faces the cylinder, _C_, around which the tracing paper is
wrapped, and which rotates once in twenty-four hours by the movement of a
clock. Mr. Hartnup, Director of the Liverpool Observatory, in his Annual
Report, 1868, says:--"For one inch change in the mercurial column the
pencil is moved through five inches, so that the horizontal lines on the
tracing, which are half an inch apart, represent one-tenth of an inch
change in the barometer. The vertical lines are hour lines, and being
nearly three-quarters of an inch apart, it will be seen that the smallest
appreciable change in the barometer, and the time of its occurrence, are
recorded."

"It has been remarked by persons in the habit of reading barometers with
large tubes, that, in squally weather, sudden and frequent oscillations
of the mercurial column are sometimes seen. Now, to register these small
oscillations must be a very delicate test of the sensitiveness of a
self-registering barometer, as the time occupied by the rise and fall of
the mercury in the tube in some cases does not exceed one minute." Mr.
Hartnup affirms that the tracing of this instrument exhibits such
oscillations whenever the wind blows strong and in squalls.

As the barometer in this instrument is precisely similar to the "Long
Range Barometer" invented by Mr. McNeild (and which will be found
described at page 48), it may be desirable to quote the following, from
Mr. Hartnup's Report:--"Mr. King constructed a small model instrument to
illustrate the principle. This instrument was entrusted to my care for
examination, and it was exhibited to the scientific gentlemen who visited
the Observatory in 1854, during the meeting of the British Association for
the Advancement of Science."


=36. Syphon, with Photographic Registration.=--A continuous
self-registering barometer has been constructed, in which photography is
employed. Those who may wish to adopt a similar apparatus, or thoroughly
to understand the arrangements and mode of observation, should consult the
detailed description given in the _Greenwich Magnetical and Meteorological
Observations_, 1847. As the principles are applicable to photographic
registration of magnetic and electric as well as meteorologic variations
in instrumental indications, it would be beside our purpose to describe
fully the apparatus.

The barometer is a large syphon tube; the bore of the upper and lower
extremities, through which the surfaces of the mercury rise and fall, is
1-1/10 inch in diameter. The glass float in the open limb is attached to a
wire, which moves a delicately-supported light lever as it alters its
elevation. The fulcrum of the lever is on one side of the wire; the
extremity on the other side, at four times this distance from the fulcrum,
carries a vertical plate of opaque mica, having a small aperture. Through
this hole the light of a gas-jet shines upon photographic paper wrapped
round a cylinder placed vertically, and moved round its axis by a clock
fixed with its face horizontal. The cylinder is delicately supported, and
revolves in friction rollers. A bent wire on the axis is embraced by a
prong on the hour hand of the time-piece; therefore the cylinder is
carried round once in twelve hours. It might be arranged for a different
period of rotation.

As the cylinder rotates, the paper receives the action of the light, and a
photographic trace is left of the movements of the barometer four times
the extent of the oscillations of the float, or twice the length of the
variations in the barometric column. Certain chemical processes are
required in the preparation of the paper, and in developing the trace. The
diagram which we give on the next page, with the explanation, taken from
Drew's _Practical Meteorology_, will enable the above description to be
better understood:

[Illustration: Fig. 28.]

"_Q e_ is a lever whose fulcrum is _e_, the counterpoise _f_ nearly
supporting it; _s_ is an opaque plate of mica, with a small aperture at
_p_, through which the light passes, having before been refracted by a
cylindrical lens into a long ray, the portion only of which opposite the
aperture _p_ impinges on the paper; _d_ is a wire supported by a float on
the surface of the mercury; _G H_ is the barometer; _p_, the vertical
cylinder charged with photographic paper; _r_, the photographic trace;
_I_, the timepiece, carrying round the cylinder by the projecting arm _t_.
It is evident that the respective distances of the float and the aperture
_p_ from the fulcrum may be regulated so that the rise and fall of the
float may be multiplied to any extent required." When _only_ the lower
surface of the mercury in a syphon barometer is read, as in the instrument
just described, a correction for temperature is strictly due to the height
of the quicksilver in the _short_ tube; but this in so short a column will
rarely be sensible.




CHAPTER IV.

MOUNTAIN BAROMETERS.


=37. The Syphon Tube Mountain Barometer, on Gay Lussac's principle=,
constructed as described at page 31, and fixed in a metallic tubular
frame, forms a simple and light travelling instrument. The graduations are
made upon the frame, and it is suspended for reading by a ring at the top,
from beneath an iron tripod stand, which is usually supplied with it.
Considerable care is requisite in adjusting the verniers, so as to keep
the instrument steady and vertical. A drawback to the convenience of this
barometer is the movement of the mercury in the short limb, which is
generally not confined, and hence has every facility for becoming quickly
oxidised in travelling. To remedy this, Messrs. Negretti and Zambra so
construct the Mountain Syphon Barometer that by a simple half turn of a
screw the mercury can be confined for portability, while the lower limb
can be taken out for cleaning whenever found requisite.


=38. Mountain Barometer on Fortin's principle.=--This barometer, with
Fortin's cistern, as arranged by Messrs. Negretti and Zambra, is an
elegant, manageable, and very accurate instrument for travelling purposes,
and well adapted for careful measurement of heights. The cistern is made
large enough to receive all the mercury that will fall from the tube at
the highest attainable elevation. The screw at the bottom confines the
mercury securely for carriage, and serves to adjust the surface of the
mercury to the zero of the scale when making an observation. The vernier
reads to .002 of an inch, and slides easily on the brass frame, which is
made as small in diameter as is compatible with the size of the tube. The
tube in this barometer should be altogether without contractions, so that
the mercury will readily fall when it is set up for observation. It must
be carefully calibrated, and its internal diameter ascertained, in order
that correction may be made for capillarity. This correction, however,
should be combined with the error of graduation, and form a permanent
index error, ascertainable at any time by comparison with an acknowledged
standard barometer.

The barometer is supported in the tripod stand (furnished as part of the
instrument) when used for observation. It is suspended by placing two
studs, in the ring on the frame, in slots formed on the top of the stand,
so that it hangs freely and vertically in gimbals. To the metal top of
the stand, mahogany legs are hinged. To make the barometer portable, it
must be lifted out of the stand, sloped gently until the mercury reaches
the top, turning the screw at the bottom meanwhile; then invert and screw
until the mercury is made tight. The inverted instrument packs in the
stand, the legs being formed to fit round the frame; and receptacles are
scooped out for the cistern, thermometer, gimbals, and vernier; so that
the instrument is firmly surrounded by the wooden legs, which are held
fast together by brass rings passed over them.


[Illustration: Fig. 29.]

=39. Newman's Mountain Barometer.=--Fig. 29 is an illustration of the
mountain barometer known as Newman's. The cistern consists of two separate
compartments;--the top of the lower and the bottom of the upper, being
perfectly flat, are pivoted closely together at the centres, so that the
lower can move through a small arc, when turned by the hand. This movement
is limited by two stops. The top of the lower compartment and the bottom
of the upper have each a circular hole, through which the mercury
communicates. When the instrument is required for observation, the cistern
is turned close up to the stop marked "_open_" or "_not portable_." When
it is necessary to pack it for travelling, the mercurial column must be
allowed to fill the tube by sloping the barometer gently; then invert it,
and move the cistern to the stop marked "_shut_" or "_portable_." In this
condition, the upper compartment is completely filled with mercury, and
consequently that in the tube cannot move about, so as to admit air or
endanger the tube. Nor can the mercury pass back to the lower compartment,
as the holes are not now coincident, and the contact is made too perfect
to allow the mercury to creep between the surfaces. The tube does not
enter the lower compartment, which is completely full of mercury when the
instrument is arranged for observation. The spare capacity of the upper
cistern is sufficient to receive the mercury which descends from the tube
to the limit of the engraved scale, which in these barometers generally
extends only to about 20 inches. A lower limit could of course be given by
increasing the size of the cisterns, which it is not advisable to do
unless for a special purpose. This barometer may be had mounted in wood,
or in brass frame. If in wood, it has a brass shield, which slides round
the scale part of the frame, so as to be easily brought in front of the
tube and scale as a protection in travelling; the vernier screw, in this
case, being placed at the top of the instrument. When the scale is
graduated with true inches, the neutral point, the capacity and
capillarity corrections should be marked on the frame. The graduated
scales, however, placed on these barometers in brass frames, are usually
artificial inches, like the Kew plan of graduation; the advantage being
that one simple correction only is required, viz. one for index error and
capillarity combined, which can always be readily determined by comparison
with a standard barometer; moreover, as no adjustment of cistern is
required in reading, the instrument can be verified by artificial pressure
throughout the scale, by the plan practised at Kew, Liverpool, &c., and
already described (see p. 18).


40. NEGRETTI & ZAMBRA'S PATENT MOUNTAIN AND OTHER BAROMETERS.

This invention is intended to make mountain and other barometers of
standard accuracy stronger, more portable, and less liable to derangement,
when being carried about, than heretofore, by dispensing with the ordinary
flexible cistern containing the mercury at the bottom of the instrument,
and adapting in lieu thereof a rigid cistern constructed of glass and
iron. The cistern is composed of a glass cylinder, which is secured in a
metallic tube or frame. In order to render the cistern mercury-tight at
top and bottom, metal caps are screwed into the tube or frame, and bear
against leather washers placed between them and the edges of the glass
cylinder. The upper cap of the cistern is tapped with a fine threaded
screw to receive the iron plug or socket, into which the barometer tube is
securely fixed. The whole length of this plug has a fine screw cut upon it
by which the cistern can be screwed up or down. At the side of this plug
or socket, extending from the lower end to within half an inch of the top,
is cut a groove for admitting the air to the surface of the mercury within
the cistern when the barometer is in use. An ivory point is screwed into
the under surface of the plug, carrying the barometer tube. This ivory
point is very carefully adjusted by measurement to be the zero point of
the instrument, from which the barometer scale of inches is divided. The
surface of the mercury in the cistern is adjusted to the zero point by
screwing the cistern up or down until the ivory point and its reflected
image are in contact.

[Illustration: Fig. 30.]

The instrument (fig. 30) is shown in a state of adjustment, ready to take
an observation; but _when it is desired to render it portable, it must be
inclined, until mercury from the cistern fills the tube; the cistern must
then be screwed up on the socket_, so as to bring the face of the upper
cap against the under side of the shoulder of the cover immediately above
it; the instrument may then be carried without being liable to
derangement.

_Precautions necessary in using the Mountain Barometer._--On removing the
barometer from its case after a journey, allow it to remain with its scale
end downward, whilst the cistern is unscrewed to the extent of _one turn
of the screw_, after which slightly shake the cistern; the mercury in it
will then completely fill the end of the barometer tube, should any
portion of it have escaped therefrom.

The barometer is then inverted, and if it be desired to make an
observation, suspend it vertically from its stand by the ring at top. The
cistern must then be unscrewed, until the surface of the mercury is
brought just level with the extreme end of the ivory or zero point fixed
to the iron plug on which the glass cistern moves up and down.

Should the elevation of the place where the barometer is to be used be
considerably above the sea level, it will be well--after suspending it
from the stand--to unscrew the cistern several turns, _holding the
barometer in an oblique position_, as at great heights the mercury will
fall considerably quicker than the cistern can be unscrewed, thereby
filling it to overflowing; but by partly unscrewing the cistern first,
room is given for the reception of a fall of mercury to the extent of
several inches.

The cistern must not be unscrewed when the _Instrument is_ INVERTED _more
than_ two turns of the screw, otherwise the mercury will flow out through
the groove.

It is found safer when travelling to carry the barometer in a horizontal
position, or with its cistern end uppermost.

_To clean the Barometer._--Should at any time the mercury in the cistern
become oxidised, and reading from its surface be difficult, it can be
readily cleaned by removing the cistern and its contained mercury from the
barometer frame by unscrewing it _when in a horizontal position_; this
precaution is necessary that the mercury in the tube may not escape, and
thereby allow air to enter. The cistern must then be emptied, and with a
dry clean leather, or silk handkerchief, well cleaned.

The operation of cleaning being performed, return the cistern to the
frame, and screw it until the face is brought up against the under side of
the shoulder, still keeping the instrument _horizontal_. The cistern is
now ready for re-filling, to do which stand the barometer on end _head
downwards_, and remove the small screw at bottom; through the aperture
thus opened, pour in mercury, passing it through a paper funnel with a
very small aperture. It is well to pass the mercury through a very small
funnel two or three times before returning it to the barometer cistern, as
by this process all particles of dust or oxide adhere to the paper, and
are effectually removed.

Should any small quantity of the mercury be lost during the operation of
cleaning, it is of no importance so long as sufficient remains to allow of
adjustment to the zero point. This latter constitutes one of the great
advantages of this new instrument over the ordinary barometer; for, in the
majority of cases, after an instrument has been compared carefully with a
standard, should mercury be lost, there is no means of correcting the
error unless a standard barometer be at hand; the new barometer is, in
this respect, independent, a little mercury more or less being
unimportant.


=41. Short Tube Barometer.=--This is simply a tube shorter, as may be
required, than that necessary to show the atmospheric pressure at the sea
level. It is convenient for balloon purposes, and for use at mountain
stations, being of course a special construction.


=42. Method of Calculating Heights by the Barometer.=--The pressure of the
atmosphere being measured by the barometer, it is evident that as the
instrument is carried up a high mountain or elevated in a balloon, the
length of the column must decrease as the atmospheric pressure decreases,
in consequence of a stratum of air being left below. The pressure of air
arises from its weight, or the attraction of gravitation upon it, and
therefore the quantity of air below the barometer cistern cannot influence
the height of the column. Hence it follows that a certain relation must
exist between the difference of the barometric pressure at the foot and at
the top of a hill or other elevation, and the difference of the absolute
heights above the sea. Theoretical investigation, abundantly confirmed by
practical results, has determined that the strata of air decrease in
density in a geometrical proportion, while the elevations increase in an
arithmetical one. Hence we have a method of determining differences of
level, by observations made on the density of the air by means of the
barometer. It is beyond our purpose to explain in detail the principles
upon which this method is founded, or to give its mathematical
investigation. We append Tables, which will be useful to practical
persons,--surveyors, engineers, travellers, tourists, &c.,--who may carry
a barometer as a travelling companion.

Table I. is calculated from the formula, height in feet = 60,200 (log.
29.922 - log. B) + 925; where 29.922 is the mean atmospheric pressure at
32 deg. F., and the mean sea-level in latitude 45 deg.; and B is any other
barometric pressure; the 925 being added to avoid minus signs in the
Table.

Table II. contains the correction necessary for the mean temperature of
the stratum of air between the stations of observation; and is computed
from Regnault's co-efficient for the expansion of air, which is .002036 of
its volume at 32 deg. for each degree above that temperature.

Table III. is the correction due to the difference of gravitation in any
other latitude, and is found from the formula, _x_ = 1 + .00265 cos. 2
lat.

Table IV. is to correct for the diminution of gravity in ascending from
the sea-level.

To use these Tables: The barometer readings at the upper and lower
stations having been corrected and reduced to temperature 32 deg. F., take out
from Table I. the numbers opposite the corrected readings, and subtract
the lower from the upper. Multiply this difference successively by the
factors found in Tables II. and III. The factor from Table III. may be
neglected unless precision is desired. Finally, add the correction taken
from Table IV.

TABLE I.

_Approximate Height due to Barometric Pressure._

  +----------------------------------------------+
  |Inches.| Feet.||Inches.| Feet.||Inches.| Feet.|
  |-------+------++-------+------++-------+------|
  |  31.0 |    0 ||  28.2 | 2475 ||  25.4 | 5209 |
  |  30.9 |   84 ||    .1 | 2568 ||    .3 | 5312 |
  |    .8 |  169 ||  28.0 | 2661 ||    .2 | 5415 |
  |    .7 |  254 ||  27.9 | 2754 ||    .1 | 5519 |
  |    .6 |  339 ||    .8 | 2848 ||  25.0 | 5623 |
  |    .5 |  425 ||    .7 | 2942 ||  24.9 | 5728 |
  |    .4 |  511 ||    .6 | 3037 ||    .8 | 5833 |
  |    .3 |  597 ||    .5 | 3132 ||    .7 | 5939 |
  |    .2 |  683 ||    .4 | 3227 ||    .6 | 6045 |
  |    .1 |  770 ||    .3 | 3323 ||    .5 | 6152 |
  |  30.0 |  857 ||    .2 | 3419 ||    .4 | 6259 |
  |  29.9 |  944 ||    .1 | 3515 ||    .3 | 6366 |
  |    .8 | 1032 ||  27.0 | 3612 ||    .2 | 6474 |
  |    .7 | 1120 ||  26.9 | 3709 ||    .1 | 6582 |
  |    .6 | 1208 ||    .8 | 3806 ||  24.0 | 6691 |
  |    .5 | 1296 ||    .7 | 3904 ||  23.9 | 6800 |
  |    .4 | 1385 ||    .6 | 4002 ||    .8 | 6910 |
  |    .3 | 1474 ||    .5 | 4100 ||    .7 | 7020 |
  |    .2 | 1563 ||    .4 | 4199 ||    .6 | 7131 |
  |    .1 | 1653 ||    .3 | 4298 ||    .5 | 7242 |
  |  29.0 | 1743 ||    .2 | 4398 ||    .4 | 7353 |
  |  28.9 | 1833 ||    .1 | 4498 ||    .3 | 7465 |
  |    .8 | 1924 ||  26.0 | 4598 ||    .2 | 7577 |
  |    .7 | 2015 ||  25.9 | 4699 ||    .1 | 7690 |
  |    .6 | 2106 ||    .8 | 4800 ||  23.0 | 7803 |
  |    .5 | 2198 ||    .7 | 4902 ||  22.9 | 7917 |
  |    .4 | 2290 ||    .6 | 5004 ||    .8 | 8032 |
  |    .3 | 2382 ||    .5 | 5106 ||    .7 | 8147 |
  +----------------------------------------------+

TABLE I.--_continued_.

_Approximate Height due to Barometric Pressure._

  +-------------------------------------------------+
  |Inches.| Feet. ||Inches.| Feet. ||Inches.| Feet. |
  |-------+-------++-------+-------++-------+-------|
  | 22.6  |  8262 ||  18.9 | 12937 ||  15.2 | 18632 |
  |   .5  |  8378 ||    .8 | 13076 ||    .1 | 18805 |
  |   .4  |  8495 ||    .7 | 13215 ||  15.0 | 18979 |
  |   .3  |  8612 ||    .6 | 13355 ||  14.9 | 19154 |
  |   .2  |  8729 ||    .5 | 13496 ||    .8 | 19330 |
  |   .1  |  8847 ||    .4 | 13638 ||    .7 | 19507 |
  | 22.0  |  8966 ||    .3 | 13780 ||    .6 | 19685 |
  | 21.9  |  9085 ||    .2 | 13923 ||    .5 | 19865 |
  |   .8  |  9205 ||    .1 | 14067 ||    .4 | 20046 |
  |   .7  |  9325 ||  18.0 | 14212 ||    .3 | 20228 |
  |   .6  |  9446 ||  17.9 | 14358 ||    .2 | 20412 |
  |   .5  |  9567 ||    .8 | 14505 ||    .1 | 20597 |
  |   .4  |  9689 ||    .7 | 14652 ||  14.0 | 20783 |
  |   .3  |  9811 ||    .6 | 14800 ||  13.9 | 20970 |
  |   .2  |  9934 ||    .5 | 14949 ||    .8 | 21159 |
  |   .1  | 10058 ||    .4 | 15099 ||    .7 | 21349 |
  | 21.0  | 10182 ||    .3 | 15250 ||    .6 | 21541 |
  | 20.9  | 10307 ||    .2 | 15402 ||    .5 | 21734 |
  |   .8  | 10432 ||    .1 | 15554 ||    .4 | 21928 |
  |   .7  | 10558 ||  17.0 | 15707 ||    .3 | 22124 |
  |   .6  | 10684 ||  16.9 | 15861 ||    .2 | 22321 |
  |   .5  | 10812 ||    .8 | 16016 ||    .1 | 22520 |
  |   .4  | 10940 ||    .7 | 16172 ||  13.0 | 22720 |
  |   .3  | 11069 ||    .6 | 16329 ||  12.9 | 22922 |
  |   .2  | 11198 ||    .5 | 16487 ||    .8 | 23126 |
  |   .1  | 11328 ||    .4 | 16646 ||    .7 | 23331 |
  | 20.0  | 11458 ||    .3 | 16806 ||    .6 | 23538 |
  | 19.9  | 11589 ||    .2 | 16967 ||    .5 | 23746 |
  |   .8  | 11721 ||    .1 | 17129 ||    .4 | 23956 |
  |   .7  | 11853 ||  16.0 | 17292 ||    .3 | 24168 |
  |   .6  | 11986 ||  15.9 | 17456 ||    .2 | 24381 |
  |   .5  | 12120 ||    .8 | 17621 ||    .1 | 24596 |
  |   .4  | 12254 ||    .7 | 17787 ||  12.0 | 24813 |
  |   .3  | 12389 ||    .6 | 17954 ||  11.9 | 25032 |
  |   .2  | 12525 ||    .5 | 18122 ||    .8 | 25253 |
  |   .1  | 12662 ||    .4 | 18291 ||    .7 | 25476 |
  | 19.0  | 12799 ||    .3 | 18461 ||    .6 | 25700 |
  +-------------------------------------------------+

TABLE II.

_Correction due to Mean Temperature of the Air._

  +-------------------------------------------+
  |Mean |Factor.||Mean |Factor.||Mean |Factor.|
  |Temp.|       ||Temp.|       ||Temp.|       |
  |-----+-------++-----+-------++-----+-------|
  | 10 deg. | 0.955 || 35 deg. | 1.006 || 60 deg. | 1.057 |
  | 11  |  .957 || 36  | 1.008 || 61  | 1.059 |
  | 12  |  .959 || 37  | 1.010 || 62  | 1.061 |
  | 13  |  .961 || 38  | 1.012 || 63  | 1.063 |
  | 14  |  .963 || 39  | 1.014 || 64  | 1.065 |
  | 15  |  .965 || 40  | 1.016 || 65  | 1.067 |
  | 16  |  .967 || 41  | 1.018 || 66  | 1.069 |
  | 17  |  .969 || 42  | 1.020 || 67  | 1.071 |
  | 18  |  .971 || 43  | 1.022 || 68  | 1.073 |
  | 19  |  .974 || 44  | 1.024 || 69  | 1.075 |
  | 20  |  .976 || 45  | 1.026 || 70  | 1.077 |
  | 21  |  .978 || 46  | 1.029 || 71  | 1.079 |
  | 22  |  .980 || 47  | 1.031 || 72  | 1.081 |
  | 23  |  .982 || 48  | 1.033 || 73  | 1.083 |
  | 24  |  .984 || 49  | 1.035 || 74  | 1.086 |
  | 25  |  .986 || 50  | 1.037 || 75  | 1.088 |
  | 26  |  .988 || 51  | 1.039 || 76  | 1.090 |
  | 27  |  .990 || 52  | 1.041 || 77  | 1.092 |
  | 28  |  .992 || 53  | 1.043 || 78  | 1.094 |
  | 29  |  .994 || 54  | 1.045 || 79  | 1.096 |
  | 30  |  .996 || 55  | 1.047 || 80  | 1.098 |
  | 31  | 0.998 || 56  | 1.049 || 81  | 1.100 |
  | 32  | 1.000 || 57  | 1.051 || 82  | 1.102 |
  | 33  | 1.002 || 58  | 1.053 || 83  | 1.104 |
  | 34  | 1.004 || 59  | 1.055 || 84  | 1.106 |
  +-------------------------------------------+

TABLE III.

  +-------------------------------------------------------+
  |Latitude.|Factor.||Latitude.|Factor.||Latitude.|Factor.|
  |---------+-------++---------+-------++---------+-------|
  |   80 deg.   |0.99751||   50    |0.99954||   20    |1.00203|
  |   75    |0.99770||   45    |1.00000||   15    |1.00230|
  |   70    |0.99797||   40    |1.00046||   10    |1.00249|
  |   65    |0.99830||   35    |1.00090||    5    |1.00261|
  |   60    |0.99868||   30    |1.00132||    0    |1.00265|
  |   55    |0.99910||   25    |1.00170||         |       |
  +-------------------------------------------------------+

TABLE IV.

  +----------------------------------------------------+
  |  Height in   |Correction||  Height in   |Correction|
  |Thousand Feet.| Additive.||Thousand Feet.| Additive.|
  |--------------+----------++--------------+----------|
  |       1      |     3    ||      14      |    44    |
  |       2      |     5    ||      15      |    48    |
  |       3      |     8    ||      16      |    52    |
  |       4      |    11    ||      17      |    56    |
  |       5      |    14    ||      18      |    60    |
  |       6      |    17    ||      19      |    65    |
  |       7      |    20    ||      20      |    69    |
  |       8      |    23    ||      21      |    74    |
  |       9      |    26    ||      22      |    78    |
  |      10      |    30    ||      23      |    83    |
  |      11      |    33    ||      24      |    88    |
  |      12      |    37    ||      25      |    93    |
  |      13      |    41    ||      26      |    98    |
  +----------------------------------------------------+

EXAMPLE 1. On October 21st, 1852, when Mr. Welsh ascended in a balloon, at
3h. 30m. p.m., the barometer, corrected and reduced, was 18.85, the air
temperature 27 deg., while at Greenwich, 159 feet above the sea, the barometer
at the same time was 29.97 inches, air temperature 49 deg., the balloon not
being more than 5 miles S.W. from over Greenwich; required its elevation.

                                            Feet.

  Barometer in Balloon    18.85, Table I. = 13007
      "     at Greenwich  29.97     "         883
                                            -----
                                            12124
  Mean Temperature, 38 deg., Table II. Factor   1.012
                                            -----
                                            12269.
                                            -----
  Latitude 51-1/2 deg., Factor from Table III. .99941
                                            -----
                                            12262
  Correction from Table IV.                    38
                                            -----
                                            12300
  Elevation of Greenwich                      159
                                            -----
      "        Balloon                      12459 feet.
                                            =====

The following examples, from the balloon ascents of J. Glashier, Esq.,
F.R.S., will serve for practice.[4]

2. Ascended from Wolverhampton, 18th August, 1862, at 2h. 38m. p.m.;
barometer (in all cases corrected and reduced to 32 deg. F) was 14.868, the
temperature of the air 26 deg.; at the same time, at Wrottesley Hall, 531 feet
above the sea, in latitude 52-1/2 deg. N, the barometer was 29.46, and the
temperature of the air 65 deg.4; find the elevation of the balloon above the
sea.

  Height, 18,959 feet.

3. From the same place an ascent was made 5th September, 1862, when at 1h.
48m. p.m. barometer was 11.954, air O deg.; at Wrottesley Hall 29.38, air 56 deg.

  Height, 23,923 feet.

4. From the Crystal Palace a balloon ascent was made 20th August, 1862. At
6h. 47m. p.m. barometer was 25.55, air 50 deg.5; and at the same time at
Greenwich Observatory, at 159 feet above the sea, the barometer was 29.81,
air 63 deg.

  Height, 4,406 feet.

5. From the same place an ascent was made 8th September, 1862. At 5 p.m.,
the balloon being over Blackheath, barometer was 25.60, and the air 49 deg.5,
while at Greenwich, barometer was 29.92, air 66 deg.4.

  Height, 4,461 feet.




CHAPTER V.

SECONDARY BAROMETERS.


=43. Desirability of Magnifying the Barometer Range.=--The limits within
which the ordinary barometric column oscillates, do not exceed four inches
for extreme range, while the ordinary range is confined to about two
inches; hence it has often been felt that the public utility of the
instrument would be greatly enhanced if by any means the scale indications
could be increased in length. This object was sought to be obtained by
bending the upper part of the tube from the vertical, so that the inches
on the scale could be increased in length in proportion to the secant of
the angle it made with the vertical. This was called "the diagonal
barometer." The upper part of the tube has also been formed into a spiral,
and the scale, placed along it, is thus greatly enlarged.

But these methods of enlarging the indications cannot be so successfully
accomplished, nor so cheaply nor so elegantly, as is done by the principle
employed in the dial barometer. Hence they are not in use.


[Illustration: Fig. 31.]

=44. Howson's Long Range Barometer.=--Very recently quite a novel design
has been patented by Mr. Howson, for a long range barometer. The
construction requires neither distortion of the tube, nor mechanism for
converting a short scale into a long one; but the mercury itself rises and
falls, through an extended range, naturally, and in simple obedience to
the varying pressure of the atmosphere. The tube is fixed, but its cistern
is sustained by the mere pressure of the atmosphere. Looking at the
instrument, it seems a perfect marvel. It appears as though the cistern
with the mercury in it must fall to the ground. The bore of the tube is
wide, about an inch across. A long glass rod is fixed to the bottom of the
glass cistern, where a piece of cork or some elastic substance is also
placed. The tube is filled with mercury; the glass rod is plunged into the
tube as it is held top downwards, until the cork gets close up to the tube
and fits tightly against it. The pressure against the cork simply prevents
the mercury from coming out while the instrument is being inverted. When
it is inverted, the mercury partly falls, and forms an ordinary barometric
column. When the top is held, the cistern and glass rod, instead of
falling away, remain perfectly suspended. There is no material support to
the cistern; the tube only is fixed, the cistern hangs to it. Glass is
many times lighter than mercury. When the glass rod is introduced, it
displaces an equal volume of mercury. The glass rod, being so much lighter
than mercury, floats and sustains the additional weight of the cistern by
its buoyancy. In the mean time, the atmosphere is acting upon the mercury,
keeping up the ordinary barometric column. Supposing there is a rise in
the ordinary barometer, the atmosphere presses some more mercury up the
tube. This mercury is taken out of the cistern, which of course becomes
lighter, and therefore the rod and cistern float up a little higher, which
thus causes the column of mercury to rise still more. The increased
pressure and buoyancy thus acting together, increase the ascent in the
barometric column, as shown by the fixed scale. One inch in the barometer
might be represented by two or more inches in this instrument, according
to construction. Supposing there was a decrease of pressure, the mercury
would fall, come into the cistern, make it heavier, and increase the fall
somewhat. Friction guides, at the top of the rod, prevent it coming into
contact with the side of the tube when vertically suspended. The
illustration, Fig. 31, shows the appearance of the instrument as framed in
wood by the makers, Messrs. Negretti and Zambra.


=45. McNeild's Long Range Barometer.=--A barometer designed by a gentleman
named McNeild is on a directly opposite principle to the one just
described. The tube is made to float on the mercury in the cistern. It is
filled with mercury, inverted in the usual manner, then allowed to float,
being held vertically by glass friction points or guides. By this
contrivance, the ordinary range of the barometer is greatly increased. One
inch rise or fall in the standard barometer may be represented by four or
five inches in this instrument, so that it shows small variations in
atmospheric pressure very distinctly. As the mercury falls in the tube
with a decrease of pressure, the surface of the mercury in the cistern
rises, and the floating tube rises also, which causes an additional
descent in the column, as shown by fixed graduations on the tube. With an
increase of pressure, some mercury will leave the cistern and rise in the
tube, while the tube itself will fall, and so cause an additional ascent
of mercury. This barometer is identical in principle with King's Barograph
(see p. 34).

The construction of Howson's and McNeild's Barometers has been assigned to
Messrs. Negretti and Zambra. These instruments are usually made for
domestic purposes with a scale of from three to five, and for public use
from five to eight times the scale of the ordinary standard. Their
sensitiveness is consequently increased in an equal proportion, and they
have the additional advantage of not being affected by differences of
level in the cistern. However, these novelties have not been sufficiently
tried to determine their practical value for strictly scientific
purposes; but as weather-glasses, for showing minute changes, they are
superior to the common barometer.


=46. The Water-glass Barometer.=--If a Florence flask, having a long neck,
have a small quantity of water poured into it, and then be inverted and so
supported that the open end dips into a vessel containing water, a small
column of water will be confined in the neck of the bottle, the pressure
of which, upon the surface of the exposed water, will be equal to the
difference between the atmospheric pressure and the elasticity of the
confined air in the body of the bottle. As the pressure of the atmosphere
varies, this column will alter in height. But the elasticity of the
confined air is also subject to variations, owing to changes of
temperature. It follows, then, that the oscillations of the column are
dependent on alterations of temperature and atmospheric pressure. Such an
arrangement has been called "the Water-glass Barometer," and bears about
the same relative value to the mercurial barometer, as an exponent of
weather changes, that a cat-gut hygrometer bears to a thermometric
hygrometer, as an indicator of relative moisture.


47. SYMPIESOMETER.

Nevertheless the instrument now about to be described, depending upon
similar principles, but scientifically constructed and graduated, is a
very useful and valuable substitute for the mercurial barometer. It
consists of a glass tube, varying, according to the purposes for which the
instrument is required, from six to twenty-four inches in length. The
upper end is closed, and formed into a bulb; the lower is turned up,
formed into a cistern, and open at top, through a pipette, or cone. A
plug, moveable by a catch from below, can be made to close this opening,
so as to render the instrument portable.

[Illustration: Fig. 32.]

The upper portion of the tube is filled with air; the lower portion, and
part of the cistern, with sulphuric acid, coloured so as to render it
plainly visible. Formerly, hydrogen and oil were used. It was found,
however, that, by the process known to chemists as _osmosis_, this light
gas in time partially escaped, and the remainder became mixed with air,
the consequence being that the graduations were no longer correct. They
are more durable as at present constructed. The liquid rises and falls in
the tube with the variations of atmospheric pressure and temperature
acting together. If the pressure were constant, the confined air would
expand and contract for temperature only, and the instrument would act as
a thermometer. In fact, the instrument is regarded as such in the
manufacture; and the thermometric scales are ascertained and engraved on
the scale. A good mercurial thermometer is also mounted on the same frame.
If, therefore, at any time the mercurial and the air thermometers do not
read alike, it must evidently be due to the atmospheric pressure acting
upon the air in the tube; and it is further evident that, under these
circumstances, the position of the top of the liquid may be marked to
represent the barometric pressure at the time. In this manner a scale of
pressure is ascertained by comparison with a standard barometer, extending
generally from 27 to 31 inches.

When made correctly, these instruments agree well with the mercurial
barometer for a number of years, and their subsequent adjustment is not a
matter of much expense.

For use at sea, the liquid column is contracted at the bend. The
sympiesometer is very sensitive, and feels the alterations in the
atmospheric pressure sooner than the ordinary marine barometer.

The scale is usually on silvered brass, mounted on a mahogany or rosewood
frame, protected in front by plate glass. It is generally furnished with a
revolving register, to record the observation, in order that it may be
known whether the pressure has increased or decreased in the interval of
observation.

Small pocket sympiesometers are sometimes fitted with ivory scales, and
protected by a neat velvet-lined pasteboard or morocco case.

_How to take an Observation._--In practice, the indications of the
atmospheric pressure are obtained from the sympiesometer by noting, first,
the temperature of the mercurial thermometer; secondly, adjusting the
pointer of the pressure scale to the same degree of temperature on the
scale of the air column; thirdly, reading the height of the liquid on the
sliding scale.

_Directions for Use._--The sympiesometer should be carried and handled so
as to keep the top always upwards, to prevent the air mechanically mixing
with the liquid. Care should also be taken to screen it from casual rays
of the sun or cabin fire.


48. ANEROIDS.

The beautiful and highly ingenious instrument called by the name
_Aneroid_, is no less remarkable for the scientific principles of its
construction and action, than for the nicety of its mechanism. It is a
substitute, and perhaps the best of all substitutes, for the mercurial
barometer. As its name implies, it is constructed "without fluid." It was
invented by M. Vidi of Paris. In the general form in which it is made it
consists of a brass cylindrical case about four inches in diameter and one
and a half inch deep, faced with a dial graduated and marked similarly to
the dial-plate of a "wheel-barometer," upon which the index or pointer
shows the atmospheric pressure in inches and decimals of an inch in
accordance with the mercurial barometer. Within the case, for ordinary
sizes, is placed a flat metal box, generally not more than half an inch
thick and about two inches or a little more in diameter, from which nearly
all the air is exhausted. The top and bottom of this box is corrugated in
concentric circles, so as to yield inwardly to external pressure, and
return when the pressure is removed. The pressure of the atmosphere,
acting externally, continually changes, while the elastic pressure of the
small quantity of air within can only vary by its volume being increased
or decreased, or by change of temperature. Leaving out of consideration,
for the moment, the effect of temperature, we can readily perceive that as
the pressure is lessened upon the outside of the box, the elastic force of
the air within will force out the top and bottom of the box; and when the
outer pressure is increased they will be forced in. Thus with the varying
pressure of the atmosphere, the top and bottom of the box approach to and
recede from each other by a small quantity; but the bottom being fixed,
nearly all this motion takes place on the top. Thus the top of the box is
like an elastic cushion, which rises and falls according as the
compressing force lessens or increases. To the eye these expansions and
contractions would not be perceptible, so small is the motion. But they
are rendered very evident by a nice mechanical arrangement. To the box is
attached a strong piece of iron, kept pressed upon it by a spring at one
extremity; so that as the top of the box rises, the motion is made
sensible at the point held by the spring, and when the top descends the
spring draws the piece of iron into close contact with it. This piece of
iron acts as a lever, having its fulcrum at one extremity, the power at
the centre of the box-top, and the other extremity controlled by the
spring. Thus it is evident that the small motion of the centre of the
box-top is much increased at the spring extremity. The motion thus
obtained is communicated to a system of levers; and, by the intervention
of a piece of watch-chain and a fine spring passing round the arbour,
turns the index to the right or left, according as the external pressure
increases or decreases. Thus, when by increase of pressure the vacuum box
is compressed, the mechanism transfers the movement to the index, and it
moves to the right; when the vacuum box bulges out under diminished
pressure, the mechanical motion is reversed, and the index moves to the
left. As the index traverses the dial, it shows upon the scale the
pressure corresponding with that which a good mercurial barometer would at
the same time and place indicate; that is, supposing it correctly
adjusted.

A different and more elegant arrangement has since been adopted. A broad
curved spring is connected to the top of the vacuum box, so as to be
compressed by the top of the box yielding inward to increased pressure,
and to relax itself and the box as the pressure is lessened. The system of
levers is connected to this spring, which augments and transfers the
motion to the index, in the manner already described. Increase of pressure
causes the levers to slacken the piece of watch-chain connected with them
and the arbour of the index. The spring now uncoils, winds the chain upon
the arbour, and turns the index to the right. Decrease of pressure winds
the chain off the barrel, tightens the spiral spring, which thus turns the
index to the left. The graduations of the aneroid scale are obtained by
comparisons with the correct standard reading of a mercurial barometer,
under the normal and reduced atmospheric pressure. Reduced pressure is
obtained by placing both instruments under the receiver of an air pump.

[Illustration: Fig. 33.]

Fig. 33 represents the latest improved mechanism of an aneroid. The outer
case and the face of the instrument are removed, but the hand is attached
by its collet to the arbour. _A_ is the corrugated box, which has been
exhausted of air through the tube, _J_, and hermetically sealed by
soldering. _B_ is a powerful curved spring, resting in gudgeons fixed on
the frame-plate, and attached to a socket behind, _F_, in the top of the
box. A lever, _C_, joined to the stout edge of the spring, is connected,
by the bent lever at _D_, with the chain, _E_, the other end of which is
coiled round, and fastened to the arbour, _F_. As the box, _A_, is
compressed by the weight of the atmosphere increasing, the spring, _B_, is
tightened, the lever, _C_, depressed, and the chain, _E_, uncoiled from
_F_, which is thereby turned so that the hand, _H_, moves to the right. In
the mean while the spiral spring, _G_, coiled round _F_, and fixed at one
extremity to the frame-work and by the other to _F_, is compressed. When,
therefore, the pressure decreases, _A_ and _B_ relax, by virtue of their
elasticity; _E_ slackens, _G_ unwinds, turning _F_, which carries _H_ to
the left. Near _J_ is shown an iron pillar, cast as part of the stock of
the spring, _B_. A screw works in this pillar through the bottom of the
plate, by means of which the spring, _B_, may be so adjusted to the box,
_A_, as to set the hand, _H_, to read on the scale according to the
indications of a mercurial barometer. The lever, _C_, is composed of brass
and steel, soldered together, and adjusted by repeated trials to correct
for the effects of temperature.

A thermometer is sometimes attached to the aneroid, as it is convenient
for indicating the temperature of the air. As regards the instrument
itself, no correction for temperature can be applied with certainty. It
should be set to read with the mercurial barometer at 32 deg. F. Then the
readings from it are supposed to require no correction.

In considering the effects of temperature upon the aneroid, they are found
to be somewhat complex. There is the effect of expansion and contraction
of the various metals of which the mechanism is composed; and there is the
effect on the elasticity of the small portion of air in the box. An
increase of temperature produces greater, a diminution less elasticity in
this air. The compensation for effects of temperature is adjusted by the
process of "trial and error," and only a few makers do it well. It is very
often a mere sham. Admiral FitzRoy writes, in his _Barometer Manual_, "The
known expansion and contraction of metals under varying temperatures,
caused doubts as to the accuracy of the aneroid under such changes; but
they were partly removed by introducing into the vacuum box a small
portion of gas, as a compensation for the effects of heat or cold. The gas
in the box, changing its bulk on a change of temperature, was intended to
compensate for the effect on the metals of which the aneroid is made.
Besides which, a further and more reliable compensation has lately been
effected by a combination of brass and steel bars."

"Aneroid barometers, if often compared with good mercurial columns, are
similar in their indications, and valuable; but it must be remembered that
they are not independent instruments, that they are set originally by a
barometer, require adjustment occasionally, and may deteriorate in time,
though slowly."

"The aneroid is quick in showing the variation of atmospheric pressure;
and to the navigator who knows the difficulty, at times, of using
barometers, this instrument is a great boon, for it can be placed
anywhere, quite out of harm's way, and is not affected by the ship's
motion, although faithfully giving indication of increased or diminished
pressure of air. In ascending or descending elevations, the hand of the
aneroid may be seen to move (like the hand of a watch), showing the height
above the level of the sea, or the difference of level between places of
comparison."

In the admiral's _Notes on Meteorology_, he says, "The aneroid is an
excellent _weather glass_, if well made. Compensation for heat or cold has
lately been introduced by efficient mechanism. In its _improved_
condition, when the cost may be about L5, it is fit for measuring heights
as far as 5,000 feet with approximate accuracy; but even at the price of
L3, as a _weather-glass_ only, it is exceedingly valuable, because it can
be carried anywhere; and if now and then compared with a good barometer,
it may be relied on sufficiently. I have had one in constant use for ten
years, and it appears to be as good now as at first. For a ship of war
(considering concussion by the fire of guns), for boats, or to put in a
drawer, or on a table, I believe there is nothing better than it for use
as a common weather-glass."

Colonel Sir H. James, R.E., in his _Instructions for taking Meteorological
Observations_, says of the aneroid, "This is a most valuable instrument;
it is extremely portable. I have had one in use for upwards of ten years,
and find it to be the best form of barometer, as a "weather-glass," that
has been made."

One of the objects of Mr. Glaisher's experiments in balloons was "to
compare the readings of an aneroid barometer with those of a mercurial
barometer up to five miles." In the comparisons the readings of the
mercurial barometer were corrected for index-error and temperature. The
aneroid readings, says Mr. Glaisher, "prove all the observations made in
the several ascents may be safely depended upon, and also that an aneroid
barometer can be made to read correctly to pressures below twelve inches."
As one of the general conclusions derived from his experiments he states,
"that an aneroid barometer read correctly to the first place, and probably
to the second place of decimals, to a pressure as low as seven inches."
The two aneroids used by Mr. Glaisher were by Messrs. Negretti and Zambra.

Aneroids are now manufactured almost perfectly compensated for
temperature. Such an instrument therefore ought to show the same pressure
in the external air at a temperature say of 40 deg., as it would in a room
where the temperature at the same time may be 60 deg.; provided there is no
difference of elevation. To test it thoroughly would require an
examination and a comparison with barometer readings reduced to 32 deg. F.,
conducted through a long range of temperature and under artificially
reduced pressure. A practical method appears to be to compare the aneroid
daily, or more often, for a few weeks with the readings of a mercurial
barometer reduced to 32 deg.; and if the error so found be constant, the
object of the compensation may be assumed to be attained, particularly if
the temperature during the period has varied greatly.

_Directions for using the Aneroid._--Aneroids are generally suspended with
the dial vertical; but if they be placed with the dial horizontal, the
indications differ a few hundredths of an inch in the two positions.
Hence, if their indications are registered, they should be kept in the
same position.

The aneroid will not answer for exact scientific purposes, as it cannot be
relied upon for a length of time. Its error of indication changes slowly,
and hence the necessity of its being set from time to time with the
reading of a good barometer. To allow of this being done, at the back of
the outer case is the head of a screw in connection with the spring
attached to the vacuum box. By applying a small turnscrew to this screw,
the spring of the vacuum box may be tightened or relaxed, and the index
made to move correspondingly to the right or left on the dial. By this
means, besides being enabled to correct the aneroid at any time, "if the
measure of a height rather greater than the aneroid will commonly show be
required, it may be _re-set_ thus: When at the upper station (_within its
range_), and having noted the reading carefully, touch the screw behind so
as to bring back the hand a few inches (if the instrument will admit),
then read off and start again. _Reverse the operation when descending._
This may add some inches of measure _approximately_."--_FitzRoy._


[Illustration: Fig. 34.]

=49. Small Size Aneroids.=--The patent for the Aneroid having expired,
Admiral FitzRoy urged upon Messrs. Negretti & Zambra the desirability of
reducing the size at which it had hitherto been made, as well as of
improving its mechanical arrangement, and compensation for temperature.
They accordingly engaged skilful workmen, who, under their directions, and
at their expense, by a great amount of labour and experiment, succeeded
in reducing its dimensions to two inches in diameter, and an inch and a
quarter thick. The exact size and appearance of this aneroid are shown in
fig. 34. The compensation is carefully adjusted, and the graduations of
the dial ascertained under reduced pressure, so that they are not quite
equal, but more accurate.


=50. Watch Aneroid.=--Subsequently the aneroid has been further reduced in
size and it can now be had from an inch and a quarter to six inches in
diameter. The smallest size can be enclosed in watch cases, fig. 35, or
otherwise, so as to be adapted to the pocket. By a beautifully simple
contrivance, a milled rim is adjusted to move round with hand pressure,
and carry a fine index or pointer, outside and around the scale engraved
on the dial, or face, for the purpose of marking the reading, so that the
subsequent increase or decrease of pressure may be readily seen. These
very small instruments are found to act quite as correctly as the largest,
and are much more serviceable. Besides serving the purpose of a
weather-glass in the house or away from home, if carried in the pocket,
they are admirably suited to the exigencies of tourists and travellers.
They may be had with scale sufficient to measure heights not exceeding
8,000 feet; with a scale of elevation in feet, as well as of pressure in
inches, engraved on the dial. The scale of elevation, which is for the
temperature of 50 deg., was computed by Professor Airy, the Astronomer Royal,
who kindly presented it to Messrs. Negretti and Zambra, at the same time
suggesting its application. Moderate-sized aneroids, fitted in leathern
sling cases, are also good travelling instruments, and will be found
serviceable to pilots, fishermen, and for use in coasting and small
vessels, where a mercurial barometer cannot be employed, because requiring
too much space.

[Illustration: Fig. 35.]

Admiral FitzRoy, in a communication to the _Mercantile Marine Magazine_,
December, 1860, says:--"Aneroids are now made more portable, so that a
pilot or chief boatman may carry one in his pocket, as a railway guard
carries his timekeeper; and, thus provided, pilots cruising for expected
ships would be able to caution strangers arriving, if bad weather were
impending, or give warning to coasters or fishing boats. Harbours of
Refuge, however excellent and important, are not always accessible, even
when most wanted, as in snow, rain, or darkness, when neither land, nor
buoy, nor even a lighthouse-light can be seen."


=51. Measurement of Heights by the Aneroid.=--For measuring heights not
exceeding many hundred feet above the sea-level by means of the aneroid,
the following simple method will suffice:--

Divide the difference between the aneroid readings at the lower and upper
stations by .0011; the quotient will give the approximate height in feet.

Thus, supposing the aneroid to read at the

  Lower Station                30.385 inches.
  Upper Station                30.025
                               ------
                Difference       .360
                               ======

  Divided gives .360/.0011 = 327 feet.

As an illustration of the mode in which the aneroid should be used in
measuring heights, the following example is given:--

A gentleman who ascended Helvellyn, August 12th, 1862, recorded the
following observations with a pocket aneroid by Negretti and Zambra:--

Near 10 a.m., at the first milestone from Ambleside, found by survey to be
188 feet above the sea, the aneroid read 29.89 inches; about 1 p.m., at
the summit of Helvellyn, 26.81; and at 5 p.m., at the milestone again,
29.76. The temperature of the lower air was 57 deg., of the upper, 54 deg. Hence
the height of the mountain is deduced as follows:--

                                          Inches.

  Reading at 10 a.m.                       29.89
        "     5 p.m.                       29.76
                                           ------
              Mean                         29.825 Table I.[5]   1010
  Upper Reading                            26.81     "          3796
                                                               -----
                   Difference                                   2786
  Mean Temperature 55 deg.5, gives in Table II.                   1.048
                                                               -----
                                                                2920
  Lat. 55 deg. N., gives in Table III.                             .9991
                                                               -----
                                                                2917
                         Table IV.                                 5
                                                               -----
                   Difference of height                         2922
  Height of lower station                                        188
                                                               -----
        "   Helvellyn                                           3110

  In Sir J. Herschell's _Physical Geography_ it is given as     3115 ft.

So near an agreement is attributable to the excellence of the aneroid, and
the careful accuracy of the observer.


52. METALLIC BAROMETER.

This instrument, the invention of M. Bourdon, has a great resemblance to
the aneroid, but is much simpler in arrangement. The inventor has applied
the same principle to the construction of metallic steam-pressure gauges.
We are here, however, only concerned with it as constructed to indicate
atmospheric pressure. It consists of a long slender flattened metallic
tube, partially exhausted of air, and hermetically closed at each end,
then fixed upon its centre, and bent round so as to make the ends face
each other. The transverse section of this tube is an elongated ellipse.
The principle of action is this: interior pressure tends to straighten the
tube, external pressure causes it to coil more. Hence as the atmospheric
pressure decreases, the ends of the tube become more apart.

This movement is augmented and transferred by a mechanical arrangement of
small metallic levers to a radius bar, which carries a rack formed on the
arc of its circle. This moves a pinion, upon the arbour of which a light
pointer, or "hand," is poised, which indicates the pressure upon a dial.
When the pressure increases, the ends of the tube approach each other, and
the pointer moves from left to right over the dial. The whole mechanism is
fixed in a brass case, having a hole at the back for adjusting the
instrument to the mercurial barometer by means of a key, which sets the
pointer without affecting the levers. The dial is generally open to show
the mechanism, and is protected by a glass, to which is fitted a moveable
index.

This barometer is very sensitive, and has the advantage of occupying
little space, although it has not yet been made so small as the aneroid.
Both these instruments admit of a great variety of mounts to render them
ornamental. The metallic barometer can be constructed with a small clock
in its centre, so as to form a novel and beautiful drawing-room ornament.

Admiral FitzRoy writes, "Metallic barometers, by Bourdon, have not yet
been tested in very moist, hot, or cold air for a sufficient time. They
are dependent, or secondary instruments, and liable to deterioration. For
limited employment, when sufficiently compared, they may be very useful,
especially in a few cases of electrical changes, _not foretold or shown by
mercury_, which these seem to indicate remarkably."

They are not so well adapted for travellers, nor for measurements of
considerable elevations, as aneroids.




CHAPTER VI.

INSTRUMENTS FOR ASCERTAINING TEMPERATURE.


=53. Temperature= is the energy with which heat affects our sensation of
feeling.

Bodies are said to possess the same temperature, when the amounts of heat
which they respectively contain act outwardly with the same intensity of
transfer or absorption, producing in the one case the sensation of warmth,
in the other that of coldness. Instruments used for the determination and
estimation of temperatures are called _Thermometers_.

Experience proves that the same body always occupies the same space at the
same temperature; and that for every increase or decrease of its
temperature, it undergoes a definite dilatation or contraction of its
volume. Provided, then, a body suffers no loss of substance or peculiar
change of its constituent elements or atoms, while manifesting changes of
temperature it will likewise exhibit alterations in volume; the latter
may, therefore, be taken as exponents of the former. The expansion and
contraction of bodies are adopted as arbitrary measures of changes of
temperature; and any substance will serve for a thermometer in which these
changes of volume are sensible, and can be rendered measureable.


=54. Thermometric Substances.=--Thermometers for meteorological and
domestic purposes are constructed with liquids, and generally either
mercury or alcohol, because their alterations of volume for the same
change of temperature are greater than those of solids; while being more
manageable, they are preferred to gases. Mercury is of all substances the
best adapted for thermometric purposes, as it maintains the liquid state
through a great alteration of heat, has a more equable co-efficient of
expansion than any other fluid, and is peculiarly sensitive to changes of
temperature. The temperature of solidification of mercury, according to
Fahrenheit's scale of temperature, is -40 deg.; and its temperature of
ebullition is about 600 deg. Sulphuric ether, nitric acid, oil of sassafras,
and other limpid fluids, have been employed for thermometers.


=55. Description of the Thermometer.=--The ordinary thermometer consists
of a glass tube of very fine bore, having a bulb of thin glass at one
extremity, and closed at the other. The bulb and part of the tube contains
mercury; the rest of the tube is a vacuum, and affords space for the
expansion of the liquid. This arrangement renders very perceptible the
alterations in volume of the mercury due to changes of temperature. It is
true, the glass expands and contracts also; but only by about
one-twentieth of the extent of the mercury. Regarding the bulb, then, as
unalterable in size, all the changes in the bulk of the fluid must take
place in the tube, and be exhibited by the expansion and contraction of
the column, which variations are made to measure changes of temperature.


56. STANDARD THERMOMETER.

The peculiarities in the construction of thermometers will be best
understood by describing the manufacture of a _Standard Thermometer_,
which is one of the most accurate make, and the scale of which is divided
independently of any comparison with another thermometer. Fig. 36 is an
illustration of such an instrument, on a silvered brass scale.

[Illustration: Fig. 36]

_Selection of Tube._--In selecting the glass tube, much care is requisite
to ascertain that its bore is perfectly uniform throughout. As received
from the glass-house, the tubes are generally, in their interior, portions
of very elongated cones, so that the bore is wider at one end than at the
other. With due care, however, a proper length of tube can be selected, in
which there is no appreciable difference of bore. This is ascertained by
introducing into the tube a length of mercury of about a half or a third
of an inch, and accurately measuring it in various positions in the tube.
To accomplish this, the workman blows a bulb at one end of the tube, and
heats the bulb a little to drive out some of the air. Then, placing the
open end in mercury, upon cooling the elasticity of the enclosed air
diminishes, and the superior pressure of the atmosphere drives in some
mercury. The workman stops the process so soon as he judges sufficient
mercury has entered. By cooling or heating the bulb, as necessary, the
mercury is made to pass from one end of the tube to the other. Should the
length of this portion of mercury alter in various parts of the bore, the
tube must be rejected. If it is, as nearly as possible, one uniform
length, the tube is set aside for filling.

The _bulb_ is never blown by the breath, but by an elastic caoutchouc ball
containing air, so that the introduction of moisture is avoided. The
spherical form is to be preferred; for it is best adapted to resist the
varying pressure of the atmosphere. The bulbs should not be too large, or
the mercury will take some time to indicate sudden changes of temperature.
Cylindrical bulbs are sometimes desirable, as they offer larger surfaces
to the mercury, and enable thermometers to be made more sensitive.

The _mercury_, with which the bulb is to be filled, should be quite pure,
and freed from moisture and air by recent boiling.

_Filling the Tube._--The filling is effected by heating the bulb with the
flame of a spirit-lamp, while the open end is embedded in mercury. Upon
allowing the bulb to cool, the atmospheric pressure drives some mercury
into it; and the process of heating and cooling is thus continued until
sufficient mercury is introduced. The mercury is next boiled in the tube,
to expel any air or moisture that may be present. In order to close the
tube and exclude all air, the artist ascertains that the tube contains
the requisite quantity of mercury; then, by holding the bulb over the
spirit flame, he causes the mercury to fill the whole of the tube, and
dexterously removing it from the source of heat, he, at the same instant,
closes it with the flame of a blow-pipe. If any air remain in the tube, it
is easily detected; for if the instrument be inverted, the mercury will
fall to the extremity of the tube, if there is a perfect vacuum, unless
the tube be so finely capillary that its attraction for the mercury is
sufficient to overcome the force of gravity, in which case the mercury
will retain its position in every situation of the instrument. If,
however, the mercury fall and does not reach quite to the extremity of the
bore, some air is present, which must be removed.

_The Graduation._--The thermometer is now prepared for graduation, the
first part of which process is the determination of two fixed points.
These are given by the temperatures of melting ice and of the vapour of
boiling water. Melting ice has always the same temperature in every place
and under all circumstances; provided only that the water from which the
ice is congealed is free from salts. The temperature of the vapour of
boiling water depends upon the pressure of the atmosphere, but is always
constant for the same pressure.

The fixed point corresponding to the temperature of melting ice is called
the _freezing point_. It is obtained by keeping the bulb and the part of
the tube occupied by mercury immersed in melting ice, until the mercury
contracts to a certain point, where it remains stationary. This position
of the end of the mercury is then marked upon the tube.

The _boiling point_ is not so easily determined, for the barometer must be
consulted about the same time. The boiling apparatus is generally
constructed of copper. It consists of a cylindrical boiler, heated from
the base by a spirit lamp or charcoal fire. An open tube two or three
inches in diameter and of suitable length enters the top of the boiler.
This tube is enveloped by another fixed to the top of the boiler but not
opening into it, and so that the two tubes are about an inch apart. The
object of the outer tube is to protect the inner tube from the cold
temperature of the air. The outer tube has an opening at the top for the
admission of the thermometer, and a hole near the bottom for the escape of
steam through a spout. When the water is made to boil, the steam rises in
the inner tube, fills the space between the tubes, and escapes at the
spout. The thermometer is then passed down into the inner cylinder, and
held securely from the top by means of a piece of caoutchouc. The tubes or
cylinders should be of sufficient length to prevent the thermometer
entering the water. This is necessary because the temperature of boiling
water is influenced by any substance which it holds in chemical solution;
and, moreover, its temperature increases with the depth, owing to the
pressure of the upper stratum. The thermometer being thus surrounded with
steam, the mercury rises in the tube. As it does so, the tube should be
depressed so as always to keep the top of the mercury just perceptible.
When the temperature of the vapour is attained, the mercury ceases to
rise, and remains stationary. The position of the end of the mercury is
now marked upon the tube, and the "_boiling-point_" is obtained.


=57. Methods of ascertaining the exact Boiling Temperature.=--The normal
boiling temperature of water all nations have tacitly agreed to fix under
a normal barometric pressure of 29.922 inches of mercury, having the
temperature of melting ice, in the latitude of 45 deg., and at the sea-level.
If the atmospheric pressure at the time or place of graduating a
thermometer does not equal this, the boiling temperature will be higher or
lower according as the pressure is greater or less. Hence a reading must
be taken from a reliable barometer, which must also be corrected for
errors and temperature, and reduced for latitude, in order to compare the
actual atmospheric pressure at the time with the assumed normal pressure.
Tables of vapour tension, as they are termed, have been computed from
accurate experimental investigations and theory,--giving the temperatures
of the vapour of water for all probable pressures; Regnault's, the most
recent, is considered the most accurate; and his investigations are based
upon the standard pressure given above, and are for the same latitude. His
Table, therefore, will give the temperature on the thermometric scale
corresponding to the pressure.

The Commissioners appointed by the British Government to construct
standard weights and measures, decided that the normal boiling-point,
212 deg., on the thermometer should represent the temperature of steam
generated under an atmospheric pressure equal in inches of mercury, at the
temperature of freezing water, to 29.922 + (cos. 2 latitude x .0766) +
(.00000179 x height in feet above the sea-level). Hence, at London, lat.
51 deg.30' N., we deduce 29.905 as the barometric pressure representing the
normal boiling point of water,--the trifling correction due to height
being neglected. If then, in the latitude of London, the barometric
pressure, at the time of fixing the boiling point, be not 29.905 inches,
that point will be higher or lower, according to the difference of the
pressure from the normal. Near the sea-level about 0.59 inch of such
difference is equivalent to 1 deg. Fahrenheit in the boiling point.

Suppose, then, the atmospheric pressure at London to be 30.785 inches, the
following calculation gives the corresponding boiling temperature for
Fahrenheit's scale:--

  Observed pressure    30.785
  Normal       "       29.905
                       ------
  Difference             .880
                      =======

As 0.59 is to 0.88, so is 1 deg. to 1 deg.5.

That is, the water boils at 1 deg.5 above its normal temperature; so that, in
this case, the normal temperature to be placed on the scale, viz. 212 deg.,
must be 1 deg.5 lower than the mark made on the tube at the height at which
the mercury stood under the influence of the boiling water.

The temperature of the vapour of boiling water may be found, at any time
and place, as follows:--Multiply the atmospheric pressure by the factor
due to the latitude, given in the annexed Table V., and with the result
seek the temperature in Table VI.

        TABLE V.                         TABLE VI.

  +----------------------------------------------------------------+
  |Latitude.| Factor. |||Temperature|Tension.||Temperature|Tension.|
  |         |         ||| of Vapour.|        || of Vapour.|        |
  |---------+---------+++-----------+--------++-----------+--------|
  |Degrees. |         ||| Degrees.  |Inches. || Degrees.  |Inches. |
  |    0    | 0.99735 |||    179    | 14.934 ||    197    | 22.036 |
  |    5    | 0.99739 |||    180    | 15.271 ||    198    | 22.501 |
  |   10    | 0.99751 |||    181    | 15.614 ||    199    | 22.974 |
  |   15    | 0.99770 |||    182    | 15.963 ||    200    | 23.456 |
  |   20    | 0.99797 |||    183    | 16.318 ||    201    | 23.946 |
  |   25    | 0.99830 |||    184    | 16.680 ||    202    | 24.445 |
  |   30    | 0.99868 |||    185    | 17.049 ||    203    | 24.952 |
  |   35    | 0.99910 |||    186    | 17.425 ||    204    | 25.468 |
  |   40    | 0.99954 |||    187    | 17.808 ||    205    | 25.993 |
  |   45    | 1.00000 |||    188    | 18.197 ||    206    | 26.527 |
  |   50    | 1.00046 |||    189    | 18.594 ||    207    | 27.070 |
  |   55    | 1.00090 |||    190    | 18.998 ||    208    | 27.623 |
  |   60    | 1.00132 |||    191    | 19.409 ||    209    | 28.185 |
  |   65    | 1.00170 |||    192    | 19.828 ||    210    | 28.756 |
  |   70    | 1.00203 |||    193    | 20.254 ||    211    | 29.335 |
  |   75    | 1.00230 |||    194    | 20.688 ||    212    | 29.922 |
  |   80    | 1.00249 |||    195    | 21.129 ||    213    | 30.515 |
  |         |         |||    196    | 21.578 ||    214    | 31.115 |
  +----------------------------------------------------------------+

_How to use the Tables._--When the _temperature_ is known to decimals of a
degree, take out the tension for the degree, and multiply the difference
between it and the next tension by the decimals of the temperature, and
add the product to the tension, for the degree.

Required the tension corresponding to 197 deg.84.

    deg.
  197           = 22.036        .465 x .84 =   .391
  198           = 22.501         197 deg.      = 22.036
                  ------                     ------
    Difference      .465         197.84    = 22.427
                  ======                     ======

When the _tension_ is given, take the difference between it and the next
less tension in the Table, and divide this difference by the difference
between the next less and next greater tensions. The quotient will be the
decimals to add to the degree opposite the next less tension.

Thus, for 23.214 inches, required the temperature.

  Given 23.214             Next greater         23.456
        22.974             Next less            22.974
        ------                                  ------
          .240                   Difference       .482
                     .240
                 And ----                    =      .5
                     .482
      Temperature opposite next less             199.0
                                                 -----
      Temperature required                       199.5
                                                 =====

A similar method of interpolation in taking out numerical quantities is
applicable to almost all tables; and should be practised with all those
given in this work.

_Example._--Thus, in Liverpool, lat. 53 deg. 30' N., the barometer reading
29.876 inches, its attached thermometer 55 deg., and the correction of the
instrument being + .015 (including index error, capillarity and capacity),
what temperature should be assigned for the boiling point marked on the
thermometer?

  Observed barometer               29.876
  Correction                      +  .015
                                   ------
                                   29.891
  Correction for temperature      -  .074
                                   ------
  Reduced reading                  29.817
  Factor from Table V.            1.00077
                                  -------
                                   208719
                                  208719
                               29817
                               -----------
  Equivalent for lat. 45 deg.      29.83995909
                               ===========

In Table VI., 29.84 gives temperature 211 deg.86.


=58. Displacement of the Freezing Point.=--Either the prolonged effect of
the atmospheric pressure upon the thin glass of the bulbs of thermometers,
or the gradual restoration of the equilibrium of the particles of the
glass after having been greatly disturbed by the operation of boiling the
mercury, seems to be the cause of the freezing points of standard
thermometers reading from a few tenths to a degree higher in the course of
some years, as has been repeatedly observed. To obviate this small error,
it is our practice to place the tubes aside for about six months before
fixing the freezing point, in order to give time for the glass to regain
its former state of aggregation. The making of accurate thermometers is a
task attended with many difficulties, the principal one being the
liability of the zero or freezing point varying constantly, so much so,
that a thermometer that is perfectly correct to-day, if immersed in
boiling water, will be no longer accurate; at least, it will take some
time before it again settles into its normal state. Then, again, if a
thermometer is recently blown, filled, and graduated immediately, or, at
least, before some months have elapsed, though every care may have been
taken with the production of the instrument, it will require some
correction; so that the instrument, however carefully made, should from
time to time be plunged into finely-pounded ice, in order to verify the
freezing point.


=59. The Scale.=--The two fixed points having been determined, it is
necessary to apply the scale. The thermometers in general use in the
United Kingdom, the British Colonies, and North America are constructed
with Fahrenheit's scale. Fahrenheit was a philosophical instrument maker
of Amsterdam, who, about the year 1724, invented the scale which has given
his name to the thermometer. The freezing point is marked 32 deg., the boiling
point 212 deg., so that the intermediate space is divided into 180 equal
parts, called degrees. "The principle which dictated this _peculiar
division_ of the scale is as follows:--When the instrument stood at the
greatest cold of Iceland, or 0 degree, it was computed to contain 11124
equal parts of quicksilver, which, when plunged in melting snow, expanded
to 11156 parts; hence the intermediate space was divided into 32 equal
portions, and 32 was taken as the freezing point of water: when the
thermometer was plunged in boiling water, the quicksilver was expanded to
11336; and therefore 212 deg. was marked as the boiling point of that fluid.
In _practice_, Fahrenheit determined the divisions of his scale from two
fixed points, the freezing and boiling of water. _The theory_ of the
division, if we may so speak, was derived from the lowest cold observed in
Iceland, and the expansions of a given portion of mercury" (_Professor
Trail_).

The divisions of the scale can be carried beyond the fixed points, if
requisite, by equal graduations. Fahrenheit's scale is very convenient in
some respects. The meteorological observer is seldom troubled with
negative signs, as the zero of the scale is much below freezing. Again,
the divisions are more numerous, and consequently smaller, than on other
scales in use; and the further subdivision into tenths of degrees, seems
to give all the minuteness usually required.

_Celcius_, a Swede, in 1742, proposed zero for the freezing point, and 100
for the boiling point, all temperatures below zero being distinguishable
by the sign (--) minus. This scale is known as the _centigrade_, and is in
use in France, Sweden, and the southern part of Europe. It has the
advantage of the decimal notation, with the embarrassment of the negative
sign.

_Reaumur_, a Frenchman, proposed zero for the freezing point, and 80 deg. for
the boiling point, an arrangement inferior to the centigrade. It is,
however, in use in Spain, Switzerland, and Germany.

It is merely a simple arithmetical operation to change the indications of
any one of these scales into the equivalents on the others. To facilitate
such conversions, tables are convenient, when a large number of
observations are under discussion; and they can be easily formed or
obtained.

In the absence of such tables, the following formulae will insure accuracy
of method, and save thinking, when occasional conversions are wanted to be
made:--F. stands for Fahrenheit, C. for Centigrade, and R. for Reaumur.

  Given.   Required.     Solution.
    F.        C.     =  (F.-32) 5/9
    F.        R.     =  (F.-32) 4/9
    C.        F.     =  9/5 C. + 32
    C.        R.     =  4/5 C.
    R.        F.     =  9/5 R. + 32
    R.        C.     =  5/4 R.

_Example._--Convert 25 deg. of Fahrenheit's scale into the corresponding
temperature on the Centigrade scale.

  Here C. = (25 - 32) 5/9
       C. = -35/9 = -3.9

or nearly 4 deg. _below_ zero of the Centigrade scale. The algebraical sign
must be carefully attended-to in the calculations.


=60. The method of testing Thermometers= for meteorological purposes is
very simple. Such thermometers are seldom required to read above 120 deg. In
these the freezing point having been determined, the divisions of the
scale are ascertained by careful comparisons, with a standard thermometer,
in water of the requisite temperature. "For the freezing point, the bulbs,
and a considerable portion of the tubes of the thermometers, are immersed
in pounded ice. For the higher temperatures, the thermometers are placed
in a cylindrical glass vessel containing water of the required heat: the
scales of the thermometers intended to be tested, together with the
Standard with which they are to be compared, are read through the glass.
In this way the scale readings may be tested at any required degree of
temperature, and the usual practice is to test them at every ten degrees
from 32 deg. to 92 deg. of Fahrenheit."--_FitzRoy._


=61. Porcelain Scale Plates.=--Thermometer scales of brass, wood, or
ivory, either by atmospheric influence or dipping in sea-water, are very
liable to become soiled and discoloured, so much so that after a very
little time the divisions are rendered nearly invisible. To obviate this
inconvenience, Messrs. Negretti and Zambra were the first to introduce
into extensive use thermometer and barometer scale-plates made of
porcelain, having the divisions and figures engraved thereon by means of
fluoric acid, and permanently burnt-in and blackened, so as always to
present a clear legible scale. That these scales have been found superior
to all others, may be inferred from the fact that all the thermometers now
supplied to the various government departments are provided with such
scales.

They can be adapted to replace any of the old forms of brass or zinc
scales, the divisions and figures of which have become obliterated or
indistinct.


=62. Enamelled Tubes.=--Nearly all thermometer tubes are now made with
enamelled backs. This contrivance of enamelling the backs of the tubes
enables the makers to use finer threads of mercury than had before been
found practicable; for were it not for the great contrast between the dark
thread of mercury and the white enamel on the glass, many of the
thermometers now in use would be positively illegible. The enamelling of
thermometers is an invention of Messrs. Negretti and Zambra. It is
necessary to state this, as many persons, from interested motives, are
anxious to ignore to whom the credit of the invention is due.


=63. Thermometers of extreme Sensitiveness.=--Thermometers for delicate
experiments are no novelty. Thermometers have been made with very delicate
bulbs to contain a very small quantity of mercury. Such instruments have
also been made with spiral or coiled tubular bulbs, but the thickness of
glass required to keep these coils or spirals in shape, and in fact to
prevent their falling to pieces, served to nullify the effect sought to be
produced, viz. instantaneous action; and where a small thin bulb was
employed, the indicating column was generally so fine that it was
positively invisible except by the aid of a powerful lens. Messrs.
Negretti and Zambra have now introduced a new form of thermometer, which
combines sensitiveness and quickness of action, together with a good
visible column. The bulb of this thermometer is of the gridiron form. Care
has been taken in constructing the bulb, so that the objections attending
spirals and other forms have been overcome; for whilst the reservoir or
bulb is made of glass so thin that it is only by a spirit lamp and not a
glass blower's blowpipe that it can be formed, yet it is still so rigid
(owing to its peculiar configuration) that no variations in its
indications can be detected, whether it be held in a horizontal, vertical,
or oblique position, nor will any error be detected if it be stood on its
own bulb. They have made thermometers with bulbs or reservoirs formed of
about nine inches of excessively thin cylindrical glass, whose outer
diameter is not more than a twentieth of an inch; so that, owing to the
large surface presented, the indications are positively instantaneous.
This form of thermometer was constructed expressly to meet the
requirements of scientific balloon ascents, to enable thermometrical
readings to be taken at the precise elevation. It was contemplated to
procure a metallic thermometer, but on the production of this perfect
instrument the idea was abandoned.


64. VARIETIES OF THERMOMETERS.

Fig. 37 is an illustration of boxwood scale thermometers for general use
and common purposes.

Fig. 38, Negretti and Zambra's Travelling Thermometer; it is fixed in a
plated metal (silver or otherwise) case, similar to a pencil-case, and has
the scale divided upon its stem.

Fig. 39, Thermometer mounted on a slab of glass, upon which the scale is
etched, the back being either oak, mahogany, or ebony.

Fig. 40, Portable Thermometer, in a bronzed brass or German silver
revolving case.

Fig. 41, Pocket Thermometer, on ivory or metallic scale, in morocco or
papier-mache case.

[Illustration: Fig. 37.]

[Illustration: Fig. 38.]

[Illustration: Fig. 39.]

[Illustration: Fig. 40.]

[Illustration: Fig. 41.]

Fig. 42, an Ornamental Drawing-room Thermometer, on ebony or ivory stand,
with glass shade.

Fig. 43, representation of highly carved or engine-turned design for
thermometer mounts, in ivory or wood, for the drawing-room. Some have the
addition of a sundial or compass at the top; they may also be formed for a
watch-stand.

Fig. 44, =Bath Thermometer=, having a float to admit of its being kept in
the water.

[Illustration: Fig. 42.]

[Illustration: Fig. 43.]

[Illustration: Fig. 44.]

Fig. 45, Thermometer with ivory scale in glass cylinder, mounted on oak
bracket with metal top, for out-door use; as at a window.

Fig. 46, Thermometer for the window, on patent porcelain or glass scale,
with oak bracket and convenient brass supports, for placing the instrument
at any angle.

Fig. 47, =Chemical Thermometer=, on boxwood scale, jointed near the bulb
on a brass hinge, ranging from 300 deg. to 600 deg.

Fig. 48, =Chemical Thermometer=, for acids, graduated on its own stem,
suitable for insertion in the tubulure of retorts; they are also made
insulated in glass cylinder to protect the graduated stem; ranging from 0 deg.
to 600 deg.

[Illustration: Fig. 45.]

[Illustration: Fig. 46.]

[Illustration: Fig. 47.]

[Illustration: Fig. 48.]

[Illustration: Fig. 49.]

[Illustration: Fig. 50.]


=65. Superheated Steam Thermometer.=--The great advantage gained by the
use of superheated steam in marine and other steam-engines being now
generally admitted by engineers, reliable thermometers, reading to 600 deg. at
least, are of the utmost importance. To meet this want, Messrs. Negretti
and Zambra have constructed for the purpose a substantial form of
thermometer, on their patent porcelain scales, in strong and convenient
metal mountings, with perforated protection to the bulb. The scales cannot
be deteriorated by steam, heat, oil, or dirt; and an occasional wiping
will be all that is necessary to keep the divisions and figures clean and
visible for any length of time; while careful calibration of the
thermometer tubes ensures the most accurate indications attainable. These
thermometers are illustrated by figs. 49 & 50. A similar, but cheaper,
construction is given to thermometers to be used with hot air, or hot
water, apparatus.


=66. Thermometer for Sugar Boiling= is protected by a metallic frame; and
is usually from three to four feet long, the graduations being confined to
a space of about twelve inches at the upper part of the instrument,
allowing the bulb and greater part of the tube to be immersed in the
boiling sugar. The graduations extend to 270 deg. or further. An index is
sometimes attached to the scale, which may be set to any degree of heat
required to be maintained.


67. EARTH THERMOMETER.

The Earth Thermometer is for ascertaining the temperature of the soil at
various depths. It is protected by a brass frame, pointed and strengthened
at the end to facilitate insertion into the ground, as in fig. 51.

[Illustration: Fig. 51.]

_Utility of a Knowledge of the Temperature of the Soil._--The temperature
of the soil is an important element in the consideration of climate, as it
concerns the vegetable kingdom.

Dr. Daubeny, in his _Lectures on Climate_, gives the following statement
with respect to some temperatures which have been observed just beneath
the earth's surface, in different parts of the globe:--

  --------------------------------------------------------------------
     Country.      |          Temperature.          |   Authority.
  -----------------+--------------------------------------------------
  Tropics, often   |162-184 deg.                        | Humboldt.
                   |                                |
  Egypt            |133-144                         | Edwards & Colin.
                   |                                |
  Orinoco          |In white sand, 140              | Humboldt.
                   |                                |
  Chili            |113-118, among dry grass        | Boussingault.
                   |                                |
  Cape of Good Hope|150, under the soil of a bulb   | Herschell.
                      garden                        |
                   |                                |
  Bermuda          |142, thermometer barely covered | Emmet.
                   |  in earth                      |
                   |                                |
  China            |Water of the fields, 113;       | Meyer.
                   |  adjacent sand, much higher;   |
                   |  blackened sides of the boat   |
                   |  at midday, 142-150            |
                   |                                |
  France           |118-122, and in one instance 127| Arago.
  --------------------------------------------------------------------

"The importance of this to vegetation may be estimated by the following
considerations:--

"It is known that every plant requires a certain amount of heat, varying
in the case of each species, for the renewal of its growth, at the
commencement of the season.

"Now when this degree of heat has spurred into activity those parts that
are above ground, and caused them to elaborate the sap, it is necessary
that the subterranean portions should at the same time be excited by the
heat of the ground to absorb the materials which are to supply the plant
with nourishment. Unless the latter function is provided for, the aerial
portions of the plant will languish from want of food to assimilate.
Indeed, it is even advisable that the roots should take the start of the
leaves, in order to have in readiness a store of food for the latter to
draw upon." In another place the professor remarks:--"It has been
calculated by Mr. Raikes, from experiments made at Chat Moss, that the
temperature of the soil when drained averages 10 deg. more than it does when
undrained; and this is not surprising, when we find that 1 lb. of water
evaporated from 1,000 lbs. of soil will depress the whole by 10 deg., owing to
the latent heat which it absorbs in its conversion into vapour."


68. MARINE THERMOMETER.

This instrument is a special construction to meet the requirements of
navigation. It consists of a carefully constructed thermometer divided on
its stem to degrees, which are sufficiently large to admit of subdivision
into tenths of degrees by estimation, and ranging from 0 deg. to 130 deg. The
scale is porcelain, having the degrees etched upon it, and burnt-in a
permanent black. The instrument is made to slide into a japanned metallic
case, for handy use and protection. It is therefore adapted for almost any
ordinary purpose; and cannot be injuriously affected by any chemical
action arising from air or sea-water. A set of these thermometers consists
of six, carefully packed in a neat box; two having japanned metallic cases
(fig. 52), the others being designed for use without the case, or to
replace a breakage.

[Illustration: Fig. 52.]

This thermometer is employed in the Royal Navy, and for the observations
made at sea for the Board of Trade.

The thermometer is now considered a necessary instrument on board ship.
Not only is it of invaluable utility in connection with the barometer as a
guide to the weather, but its indications are of service in showing the
presence of a warm or cold current in the sea; many of the great oceanic
currents being characterised by the warmth or coldness of their waters. In
seas visited by icebergs, the habitual use of the thermometer would
indicate their proximity, as the water is rendered colder for some
distance around by the thawing of huge masses of ice. The water over a
shoal in the sea is generally colder than the surface-water of the
surrounding ocean; which may result from the cold water being brought to
the surface by the current of water encountering the shoal. With this fact
navigators are well acquainted; and therefore a fall in the sea-water
thermometer may forebode that shallow water is at hand. It has been
ascertained that fish inhabit regions of the oceans and seas having the
peculiar temperature suitable to their habits. The better and firmer sort
of fish are found where cold waters exist. Those taken in warmer belts or
streams of water, even in the same latitude, are far inferior in
condition, and less approved by the palate. The fish of the Mediterranean,
a warm sea, are generally poor and scarce. Fish taken in the cold waters
between the American shore and the Gulf Stream are much esteemed; while in
and on the other side of the stream they are said to be tasteless, and of
no flavour. Between the coasts of China and the warm waters of the
Japanese current, the seas abound with excellent fish; but in the warm
waters of the current and beyond, they are never seen in such shoals.

In fact, it is clearly ascertained that fishes are adapted to climates,
like birds and beasts. It has been even affirmed, after careful
investigation, that herrings, which abound in the British Seas, and form a
most important branch of our fisheries, can only be found in a temperature
varying from 54 deg. to 58 deg. Hence the thermometer, if brought into use by the
fishermen, would guide them to the spots where they may with the best
chance cast their nets on dark nights, when other indications are not
perceptible.

This thermometer in its metallic case is perfectly suited for dipping
overboard, or placing in a bucket of water just taken from the sea, to
ascertain its temperature.




CHAPTER VII.

SELF-REGISTERING THERMOMETERS.


=69. Importance of Self-Registering Thermometers.=--Heat being apparently
the most effective agent in producing meteorological phenomena, the
determination of the highest temperature of the day, and the lowest during
the night, is a prime essential to enable an estimate of the climate of
any place to be formed. To observe these extremes by means of the ordinary
thermometer would be impracticable, from the constant watchfulness which
would be necessary. Hence, the utility and importance of self-recording
thermometers are evident. A thermometer constructed to _register_ the
highest temperature is usually called a _maximum thermometer_; one to show
the lowest temperature is termed a _minimum thermometer_; and if made to
record both extremes of temperature, it is designated a
_maximum-and-minimum thermometer_. We will, for the sake of method,
describe the instruments in use in this order.

It would carry us beyond our scope to explain in detail the methods of
dealing with temperature observations; but we may remark that half the sum
of the maximum and minimum temperature of each day of twenty-four hours,
is not what meteorologists designate the _mean daily temperature_,
although it very frequently approximates to it. The mean temperature of
the day is understood to be the average of twenty-four consecutive hourly
readings of a thermometer; and meteorology now supplies formulae whereby
this result can be deduced from two or three observations only in a day.
But we would observe that the actual mean temperature of any place has not
such an important influence upon life, either animal or vegetable, as the
abruptness and magnitude of the variations of temperature. Climate,
therefore, should be estimated more by the range of the thermometer than
by the average of its indications. The Registrar General's returns prove
that with a wide range of the thermometer, the mortality greatly
increases; and it is now becoming apparent to meteorologists that the
daily range of the thermometer marks the effects of temperature on the
health of men, and the success of crops, better than any other
meteorological fact of which we take cognizance. Now that self-registering
thermometers are constructed with mercury, the most appropriate of all
thermometric substances, not only for maxima, but likewise for minima
temperatures, the determination of the diurnal range of temperature is
rendered more certain, and observations at different places are more
strictly comparable.


MAXIMA THERMOMETERS.

=70. Rutherford's Maximum Thermometer.=--The maximum thermometer, invented
by Dr. John Rutherford, differs from an ordinary thermometer in having a
small cylinder of steel, porcelain, or aluminium, moving freely in the
tube beyond the mercury, so as to form an index. The stem of the
thermometer is fixed horizontally on the frame, which must be suspended in
the same position, as represented in fig. 53. The instrument is set by
holding it bulb downward, so as to allow the index to fall by its own
gravity into contact with the mercury. Increase of heat produces expansion
of the mercury, which consequently pushes forward the index. When the
temperature decreases, the mercury recedes from the index, leaving it so
that the extremity which was in contact with the mercury indicates upon
the scale the highest temperature since the instrument was last set.

[Illustration: Fig. 53.]

As it is easily constructed and is comparatively cheap, it is still
employed for ordinary purposes. Its disadvantages are, firstly, its
liability of soon getting out of order by the index becoming embedded in
the mercury, or fixed by oxidation, thus rendering it altogether useless;
secondly, the ease with which the index can be displaced by the wind
moving the instrument, or other accidental disturbance, so as to cause it
to give erroneous indications occasionally; and thirdly, its consequent
total unfitness for use at sea.

In the part of the tube beyond the mercury, a small quantity of air is
enclosed for the purpose of preventing the metal flowing freely in the
tube. This necessitates the construction of a larger bulb, which renders
the thermometer less sensitive. Moreover, as it frequently happens that
some mercury passes the index, particles of air insinuate themselves in
the metal, and cause separations in the column, which very often can be
removed only by a maker. To facilitate this re-adjustment, a small chamber
is left at the end of the tube, and the mercury being expanded into it by
heat until the index and air bubbles are forced into it, if possible, upon
the cooling down again, by a little management, the mercury will contract,
leaving the air and index behind. Yet sometimes the index cannot be moved
in the least from its place of fixture, so that the instrument must be
virtually reconstructed.


=71. Phillip's Maximum Thermometer.=--A maximum thermometer, better
perhaps in its action than Rutherford's, has been suggested by Professor
John Phillips, of Oxford. A small portion of air is introduced into an
ordinary thermometer, so as to cut off about half an inch of the mercurial
thread near its end in the tube. This forms a maximum thermometer, when
the stem is arranged horizontally. The isolated portion is pushed forward
by expansion, and is left in this position when the mercury contracts.
The end remote from the bulb shows on the scale the maximum temperature.

When made with a capillary tube so fine that the attraction arising from
capillarity overcomes the force of gravity, and prevents the mercury
falling to the end of the tube when the instrument is inverted, it forms a
very serviceable thermometer, quite portable and suitable for use on board
ship. In such a tube a smart shake from a swing of the hand is required to
bring the detached portion back to the column, so as to set the instrument
for future observation; no ordinary motion will move it. When the
thermometer has not this peculiarity, the mercury will flow to the end, if
held bulb downward; and in this state it is not at all a satisfactory
instrument, as the air is likely to be displaced, and a great deal of tact
is requisite to again get it to divide the column suitably. It has been
found in practice that the air bubble at different temperatures assumes
different lengths, and if very small it disappears in a few years by
oxidation and by diffusion with the mercury, so that the instrument
becomes defective and uncertain in action,--results which led to the
construction of the self-registering mercurial maximum thermometer,
invented and patented by Messrs. Negretti and Zambra. It has been before
the public about twelve years; we may therefore, now, safely speak of its
merits.


=72. Negretti and Zambra's Patent Maximum Thermometer= consists of a glass
tube containing mercury fitted on an engraved scale, as shown in fig. 54.
The part of the thermometer tube above the mercury is entirely free from
air; and at the point A in the bend above the bulb, is inserted and fixed
with the blow-pipe a small piece of solid glass, or enamel, which acts as
a valve, allowing mercury to pass on one side of it when heat is applied,
but not allowing it to return when the thermometer cools. When mercury has
been once made to pass the contraction, which nothing but the expansive
force of heat can effect, and has risen in the tube, the upper end of the
column registers the maximum temperature. To return the mercury to the
bulb, we must apply a force equal to that which raised it in the tube; the
force employed is gravity, assisted when necessary by a little agitation
of the instrument.

[Illustration: Fig. 54.]

The degrees are generally divided on the stems of these thermometers, but
their frames of course bear a scale as well. The makers have various
styles of framing in wood, metal, porcelain, and even glass. Each material
is eligible according to requirements. Porcelain scales, having the marks
_etched_ upon them by acid and permanently blackened and baked in,--by a
process for which the inventors have a separate patent,--will be found
very serviceable, as they do not corrode or tarnish by exposure to any
kind of weather; while any amount of dust and dirt can readily be cleaned
off.

The chief recommendation of this thermometer is its simplicity of
construction, enabling it to be used with confidence and safety. Of no
other maximum thermometer can it be said that it is impossible to derange
or put it out of order; hence, as regards durability, it surpasses all
others. Nothing short of actual breakage can cause it to fail. Hence it is
the most easily portable of all self-registering thermometers, an
advantage which renders it suitable for travellers, and for transmission
abroad. In the year 1852, the British Meteorological Society reported this
thermometer to be "the best which has yet been constructed for maximum
temperature, and particularly for sun observations." Since then eleven
years have elapsed, and it is still without a rival.

_Directions for use._ In using this thermometer for meteorological
observations, it should be suspended by means of two brass plates B, C,
attached for that purpose, in such manner that it hangs raised up a little
at C, and so placed that it is in the shade, with the air passing freely
to it from all sides; then, on an increase of heat, the mercury will pass
up the tube as in an ordinary thermometer, and continue doing so as long
as the heat increases. On a decrease of heat, the contraction of mercury
will take place _below_ the _bend_ in the tube, leaving the whole column
of mercury in the tube, thus registering the highest temperature, and
showing such till the instrument is disturbed.

To prepare the instrument for future observations, remove and hold it
perpendicularly, with the bulb downward, and then shake it. The mercury
will then descend in the tube, and indicate the temperature of the air at
that time; and, when again suspended, is prepared for future observation.

After the temperature has attained a maximum, there will be, with a
decrease of heat, a slight contraction of mercury in the tube--as well as
of that in the bulb--and hence doubts have arisen as to the accuracy of
the registration; but calculation shows, and critical trial has proved,
that the greatest daily range of temperature will not produce an error
large enough to be appreciable on the scale.

A very great advantage of this thermometer is that the mercury may be
allowed to flow to the end of the tube without the maximum temperature
attained during an experiment being lost. It can be employed with the bulb
uppermost. All that is necessary for reading the maximum temperature is to
slope the instrument so that the mercury flows gently towards the bulb. It
will then stop at the contraction so as to show the maximum temperature on
the scale. Afterwards the mercury is driven into the bulb by agitating the
instrument while held in the hand. Hence the instrument is invaluable as a
registering thermometer on board ship, as its indications are in no way
affected by the motions and tremors of the vessel.

For physiological experiments, such as taking the temperature of the
mouth in fever, this thermometer is the only one that can be used with
certainty, as it can be held in any position, without losing the maximum
temperature attained.


MINIMA THERMOMETERS.

=73. Rutherford's Alcohol Minimum Thermometer=, fig. 55, consists of a
glass tube, the bulb and part of the bore of which is filled with
perfectly pure spirits of wine, in which moves freely a black glass index.
A slight elevation of the thermometer, bulb uppermost, will cause the
glass index to flow to the surface of the liquid, where it will remain,
unless violently shaken. On a _decrease_ of temperature the alcohol
recedes, taking with it the glass index; on an _increase_ of temperature
the alcohol alone ascends in the tube, leaving the end of the index
_farthest_ from the bulb indicating the minimum temperature.

[Illustration: Fig. 55.]

_Directions for using, &c._--Having caused the glass index to flow to the
end of the column of spirit, by slightly tilting the thermometer, bulb
uppermost, suspend the instrument (in the shade with the air passing
freely to it on all sides) by the two brass plates attached for that
purpose,--in such manner that the bulb is about half an inch lower than
the upper, or the end of the thermometer farthest from the bulb; then, on
a decrease of temperature, the spirits of wine will descend, carrying with
it the glass index; on an increase of temperature, however, the spirits of
wine will ascend in the tube, leaving that end of the small glass index
farthest from the bulb indicating the minimum temperature. To reset the
instrument, simply raise the bulb end of the thermometer a little, as
before observed, and the index will again descend to the end of the
column, ready for future observation.

_Precautions._--1. By no means jerk or shake an alcohol minimum
thermometer _when resetting_ it, for by so doing it is liable to
disarrange the instrument, either by causing the index to leave the
spirit, or by separating a portion of the spirit from the main column.

2. As alcohol thermometers have a tendency to read lower by age, owing to
the volatile nature of the fluid allowing particles in the form of vapour
to rise and lodge in the tube, it becomes necessary to compare them
occasionally with a mercurial thermometer whose index error is known; and
if the difference be more than a few tenths of a degree, examine well the
upper part of the tube to see if any alcohol is hanging in the bore
thereof; if so, the detached portion of it can be joined to the main
column by swinging the thermometer with a pendulous motion, _bulb
downwards_.

3. The spirit column is sometimes much separated by jolting in travelling.
If the instrument is in such a condition when received, it should be held
by the right hand, bulb downward, and the frame tapped smartly, but
cautiously, against the palm of the left hand. The broken thread of spirit
will soon begin to join, and by continuing the operation a sufficient time
all the bubbles will disappear, and the thermometer become as good as
ever.


=74. Horticultural Minimum Thermometer.=--This instrument, represented in
fig. 56, is a special construction of Rutherford's minimum thermometer to
meet the requirements of horticulturists. It is desirable, if not
essential, that gardeners should have the means of ascertaining to what
temperature stoves and greenhouses descend on cold nights, especially in
winter. This thermometer is mounted on a strong cast zinc frame, with the
divisions and figures of the scale raised.

[Illustration: Fig. 56.]

The sunk surface of the frame is painted dark; the figures and division a
bright colour, so that observations can be made without a close inspection
of the instrument.

The directions for using are the same as those given in the preceding
section. It may be used as an ordinary thermometer, by simply hanging it
from the top loop, in which position, the coloured liquid will always
indicate the present temperature.

It was a source of annoyance with the ordinary boxwood and flat metal
scales, that after a time, exposure to a damp warm atmosphere favoured the
growth of confervae upon them, and obliterated the divisions; the plan of
raising the figures and divisions of the scale has been found to prevent
the destruction of the instrument in this way.


=75. Baudin's Alcohol Minimum Thermometer.=--This instrument resembles
Rutherford's thermometer in appearance; its indications are given by the
expansion and contraction of alcohol, and its minimum temperature is
likewise registered by a glass index being pulled back and left behind by
the alcohol, as in Rutherford's instrument. There is, however, a great
improvement in Baudin's instrument; for whilst Rutherford's thermometer
can only register in a horizontal position, Baudin's can be used either
horizontally or vertically, as necessity may require. This important
change is effected in the following manner:--Instead of the index in the
thermometer being loose and free to run up and down according to the
position in which the instrument is held, as in Rutherford's, the index in
the new instrument is made to fit the bore of the tube as nearly tight as
possible, so much so that in holding the thermometer even upside down, or
shaking it, the index will not shift from its position; but, inasmuch as a
minimum thermometer with an immoveable index could not be set when
required for observation, and would consequently be useless, the inventor
has introduced behind the index a piece of solid glass, about
one-and-a-half inch in length, which moves freely in the alcohol. The
addition of the weight of this piece of glass on the top of the index,
when turned upside down, forces the index down to the edge of the alcohol;
and it is there left, as in the case of the ordinary Rutherford's
thermometer. It is, therefore, by turning the thermometer upside down, and
letting the moveable piece of glass fall on the index, that the index is
driven to the end of the alcohol; after this operation the thermometer is
hung up either horizontally or vertically, and will then be ready for use.

The index, although immoveable _per se_, is by the alcohol drawn back, as
in the ordinary minimum, and its indications are read off on the scale
from the top of the index.


=76. Mercurial Minima Thermometers desirable.=--Alcohol does not expand
equally for equal increments of heat, consequently errors are likely to
exist in the scale indications unless the graduations are very
accurately--not necessarily equally--made. On this account, as well as
from the volatility of alcohol, and the intervention of gaseous partitions
in the tube, a good and thoroughly reliable minimum thermometer was for a
long time a desideratum. It was desirable to obtain a thermometer which
should register the lowest temperature by mercury, the fluid in general
use for meteorological thermometers. Several instruments have recently
been invented to meet this requirement, which are suitable and
satisfactory for land purposes, but one well adapted for use on board ship
is still very much wanted.

For very low temperatures, alcohol thermometers will always be required;
as mercury freezes at -40 deg. F, and contracts very irregularly much before
this point, while alcohol has never yet been frozen.


=77. Negretti and Zambra's Patent Mercurial Minimum Thermometer=,
represented by fig. 57, has a cylindrical bulb of large size, which, at
first sight, might induce the idea that the instrument would not be
sufficiently sensitive; but as length is given to the cylinder instead of
increasing its diameter, it will be found as sensitive as a globular bulb
of the same diameter, and much more so than an ordinary alcohol
thermometer.

[Illustration: Fig. 57.]

The reason for having the bulb large is to allow the internal diameter of
the thermometer tube to be larger than that generally used for
thermometrical purposes, so that a steel index, pointed at both ends, may
move freely within when required.

The tube is blown, filled and regulated in the usual way, 60 deg. of
temperature being about half-way up the tube. A small cylindrical bulb is
then formed at the upper end of the tube, and then is introduced a steel
needle pointed at both ends, that in contact with the mercury being
abrupt, the other more prolonged. The open extremity of the tube is now
drawn out into a fine capillary tube, and the bulb of the instrument
warmed so as to cause the mercury to fill the tube completely. When the
mercury reaches the capillary tube, the flame of a blow-pipe is applied;
the glass is dexterously melted, the superfluous part taken away, and the
tube left hermetically closed. During this operation, the steel index has
been embedded in the heated mercury. As the instrument cools, if held
upright, the mercury will recede and expose the needle, which will then
follow the descending column simply by its own gravity. In this condition
the thermometer resembles Rutherford's maximum, being a tube of mercury
with a steel index floating on its surface; but it possesses these
important advantages: it is quite free from air, so that the mercury can
move with perfect freedom; and the index is pointed at both ends, to allow
the mercury to pass, instead of being ground flat to prevent it.

_To use the Thermometer_, it is suspended perpendicularly (figure 57) with
the steel index resting on the surface of the mercurial column. As the
mercury in the cylinder contracts, that in the tube descends, and the
index, of its own gravity, follows it; on the contrary, as the mercury
expands and rises in the tube, it passes the index on one side, and in
rising, exerts a lateral pressure on the needle, and jams it to one side
of the tube, where it remains firmly fixed, leaving the upper point of the
needle indicating the minimum temperature. In this thermometer, the
reading is always from the upper point of the needle, and not from the
mercury itself.

_To extricate the Needle_ from the mercury, a magnet is used, when, if the
needle is embedded only a few degrees, it can readily be withdrawn without
altering the position of the instrument. Should the magnet not be
sufficient for the purpose, we simply turn the thermometer on its support
from the upright position, slightly elevating the bulb (fig. 58 (=2=)).
The mercury and index will then flow into the small reservoir. Should the
index not freely leave the tube with the mercury, assist it with a magnet,
and when the mercury and index are in the upper bulb (figure =2=), apply a
magnet outside, which will attract and hold fast the index; and whilst
thus holding it, again bring the thermometer to the upright position, when
the mercury will immediately fall back into the tube, leaving the index
attached to the magnet (figure =4=), with which it is guided down to the
surface of the mercury, ready for another observation.

[Illustration: Fig. 58.]

Care must be taken not to withdraw the magnet until the index is in
contact with mercury; for, if released before touching, it might plunge
too deeply, and give a false indication. The rule for re-setting it will
be to bring the needle-point in contact with the mercury, and then
withdraw the magnet, having previously ascertained that no particles of
mercury are attached to the index.

It may sometimes, though rarely, happen, that from the time a minimum
temperature is registered by the index, and by the time an observation is
made, the mercury may have risen so high in the tube as to completely pass
the index, as shown (figure =3=). Should it so happen, the space which the
index occupies will readily be observed, as it will be pressed to one side
of the tube, causing a different appearance in that part, although the
point of the needle may not be seen. If such be the case, apply a magnet
to the spot where you see the index is fixed: this will hold the needle
firmly. Then, by slightly tilting the thermometer bulb uppermost, the
mercury will flow into the top bulb, leaving the index attached to the
magnet, and quite uncovered. Having taken the reading, draw the needle
into the top bulb, and hold it there whilst you adjust the thermometer by
again bringing it to the upright position.

By contracting the bore of this thermometer, at the bend of the tube,
sufficiently to keep the mercury from flowing out of its bulb with too
much freedom by motion, the instrument becomes perfectly safe for
transmission abroad.


=78. Negretti & Zambra's Second Patent Mercurial Minimum Thermometer.=--In
this thermometer a principle is used that has been long known to
scientific men, viz. the affinity of mercury for platinum. If mercury be
placed in contact with platinum under ordinary circumstances, no effect
will take place; but if the mercury is once made to attack the platinum,
the amalgamation is permanent and the contact perfect, so much so, that
the principle was made use of in constructing standard barometers. A ring
of platinum was fused round the end of the tube, dipping into the mercury;
and the contact between the platinum and mercury became so perfect that
air could not creep down the tube and up the bore, as in ordinary
barometer tubes. This principle of adhesion or affinity of mercury for
platinum has been brought into play for the purpose of arresting the
mercury after it has reached the minimum temperature in a thermometer.
This thermometer is made as follows:--behind the bulb is placed a
supplementary chamber; in the space or neck between the bulb of the
thermometer and the chamber, is placed a small piece of platinum; this may
be of any shape or size, but the smaller the better. This is not to fit in
the neck; it must, on the contrary, be rather loose; it may be fastened in
position or not. The instrument is represented by fig. 59.

[Illustration: Fig. 59.]

_Directions for using._--Having suspended the thermometer in a horizontal
position, the mercury is made to stand in exact contact with the platinum
plug by slightly elevating the bulb end of the instrument. The thermometer
is now ready for observation. On a decrease of temperature, the mercury
will endeavour to contract first from the easier passage, viz. behind the
bulb; but in consequence of the adhesion of the mercury to the platinum,
it cannot recede from here, it is therefore forced to contract from the
indicating tube, and will continue to do so as long as the temperature
decreases; and as no indices are employed in this thermometer, the extreme
end of the mercurial column will show "how cold it has been." On an
increase of temperature the mercury will glide over the platinum plug and
expand by the easier passage into the supplementary chamber, and there
remain until a decrease of temperature again takes place, when the mercury
that had gone into the supplementary chamber will be the first to recede,
until it reaches the platinum plug, its further progress being arrested;
it will then fall in the indicating tube, and there remain until re-set.


=79. Casella's Mercurial Minimum Thermometer.=--The general form and
arrangement of this instrument is shown in fig. 60. A tube with large
bore, _a_, has at the end a _flat glass diaphragm_ formed by the abrupt
junction of a small chamber, _b c_, the inlet to which at _b_ is larger
than the bore of the indicating tube. The result of this is that on
setting the thermometer, as described below, the contracting force of the
mercury in cooling withdraws the fluid in the indicating stem only; whilst
on its expanding with heat, the long column does not move, the increased
bulk of mercury finding an easier passage into the small pear-shaped
chamber attached.

[Illustration: Fig. 60.]

We believe that a small speck of air must be confined in the chamber, _b
c_, to act as a spring to start the mercury from the chamber in the act of
setting the thermometer. Were this air not present, the mercury would so
adhere to the glass that no amount of shaking could induce it to flow from
the chamber.

_To set the Instrument_, place it in a horizontal position, with the back
plate, _d_, suspended on a nail, and the lower part supported on a hook,
_e_. The bulb end may now be gently raised or lowered, causing the mercury
to flow slowly until the bent part, _a_, _is full_ and the chamber, _b c_,
_quite empty_. At this point the flow of mercury in the long stem of the
tube is arrested, _and indicates the exact temperature_ of the bulb or air
at the time. On an increase of temperature the mercury will expand into
the small chamber, _b c_; and a return of cold will cause its recession
from this chamber only, until it reaches the diaphragm, _b_. Any further
diminution of heat withdraws the mercury down the bore to whatever degree
the cold may attain, where it remains until farther withdrawn by increased
cold, or till re-set for future observation.


MAXIMA AND MINIMA THERMOMETERS.

=80. Rutherford's= arrangement for obtaining a complete instrument for the
registration of heat and cold was simply mounting a maximum thermometer
and a minimum thermometer upon the same frame or slab. Thus constructed,
they are often called "day and night" thermometers, though somewhat
inappropriately; for in temperate climates the temperature of the night
sometimes exceeds that of the day, notwithstanding the reverse is the
general law of temperature. Fig. 61 will explain the arrangement of
Rutherford's day and night thermometer.

[Illustration: Fig. 61.]


=81. Sixe's Self-Registering Thermometer.=--The very ingenious and
certainly elegant instrument about to be described was invented by James
Sixe, of Colchester. It consists of a long cylindrical bulb, united to a
tube of more than twice its length, bent round each side of it in the form
of a syphon, and terminated in a smaller, oval-shaped bulb. Figure 62
gives a representation of this instrument. The lower portion of the syphon
is filled with mercury; the long bulb, the other parts of the tube, and
part of the small bulb, with highly rectified alcohol. A steel index moves
in the spirit in each limb of the syphon. The two indices are terminated
at top and bottom with a bead of glass, to enable them to move with the
least possible friction, and without causing separation of the spirit, or
allowing mercury to pass easily. They would, from their weight, always
rest upon the mercury; but each has a fine hair tied to its upper
extremity and bent against the interior of the tube, which acts as a
spring with sufficient elasticity to keep the index supported in the
spirit in opposition to gravity.

[Illustration: Fig. 62.]

The instrument acts as follows:--A rise of temperature causes the spirit
in the long bulb to expand and press some of the mercury into the other
limb of the syphon, into which it rises also from its own expansion, and
carries the index with it, until the greatest temperature is attained. The
lower end of this index then indicates upon the engraved scale the maximum
temperature. As the temperature falls the spirit and the mercury contract,
and in returning towards the bulb the second index is met and carried up
by the mercury until the lowest temperature occurs, when it is left to
indicate upon the scale the minimum temperature. The limb of the syphon
adjoining the bulb requires, therefore, a descending scale of
thermometric degrees; the other limb, an ascending scale. The graduations
must be obtained by comparisons with a standard thermometer under
artificial temperatures, which should be done in this way for every 5 deg., in
order to correct for the inequality in the bore of the tube, and the
irregular expansion of the spirit. The instrument is set for observation
by bringing the indices into contact with the mercury, by means of a small
magnet, which attracts the steel through the glass, so that it is readily
drawn up or down. They should be drawn nearly to the top of the limbs when
it is desired to remove the instrument, which should be carefully carried
in the vertical position; for should it be inverted, or laid flat, the
spirit may get among the mercury, and so break up the column as to require
the skill of a maker to put it in order again. For transmission by
ordinary conveyances, it requires that attention be given to keep it
vertical. The entanglement of a small portion of mercury with the indices
is sometimes a source of annoyance in this instrument, for the readings
are thereby rendered somewhat incorrect. Small breakages in the mercury,
either from intervening bubbles of spirit or adhesion to the indices, may
generally be rectified by cautiously tapping the frame of the instrument,
so as to cause the mercury to unite by the assistance thus given to its
superior gravity.

These thermometers, when carefully made and adjusted to a standard
thermometer, are strongly recommended for ordinary purposes, where strict
scientific accuracy is not required. This is also the only fluid
thermometer applicable for determining the temperature of the sea at
depths.




CHAPTER VIII.

RADIATION THERMOMETERS.


=82. Solar and Terrestrial Radiation considered.=--The surface of the
earth absorbs the heat of the sun during the day, and radiates heat into
space during the night. The envelope of gases and vapour, which we call
the atmosphere, exerts highly important functions upon these processes.
Thanks to the researches of Professor Tyndall, we are now enabled to
understand these functions much more clearly than heretofore. His
elaborate, patient, and remarkably sagacious series of experiments upon
radiant heat, have satisfactorily demonstrated that _dry_ air is as
transparent to radiant heat as the vacuum itself; while air _perfectly
saturated_ with aqueous vapour absorbs more than five per cent. of radiant
heat, estimated by the thermal unit adopted for the galvanometer
indications of the effect upon a thermo-electric pile.

Aqueous vapour, in the form of fog or mist, as is well known, gives to our
sensation a feeling of cold, and interferes with the healthy action of the
skin and the lungs; the cause being its property of absorbing heat from
our person.

Air containing moisture in an invisible state likewise exerts a remarkable
influence in radiating and absorbing heat. By reason of these properties,
aqueous vapour acts as a kind of blanket upon the ground, and maintains
upon it a higher temperature than it would otherwise have. "Regarding the
earth as a source of heat, no doubt at least ten per cent. of its heat is
intercepted within ten feet of the surface." Thus vapour--whether
transparent and invisible, or visible, as cloud, fog, or mist--is
intimately connected with the important operations of solar and
terrestrial radiation. Cloudy, or humid days, diminish the effect upon the
soil of solar radiation; similar nights retard the radiation from the
earth. A dry atmosphere is the most favourable for the direct transmission
of the sun's rays; and the withdrawal of the sun from any region over
which the air is dry, must be followed by very rapid cooling of the soil.
"The removal, for a single summer night, of the aqueous vapour from the
atmosphere which covers England, would be attended by the destruction of
every plant which a freezing temperature could kill. In Sahara, where 'the
soil is fire and the wind is flame,' the refrigeration at night is often
painful to bear. Ice has been formed in this region at night. In
Australia, also, the _diurnal range_ of temperature is very great,
amounting, commonly, to between 40 and 50 degrees. In short, it may be
safely predicted, that wherever the air is _dry_, the daily thermometric
range will be great. This, however, is quite different from saying that
when the air is _clear_, the thermometric range will be great. Great
clearness to light is perfectly compatible with great opacity to heat; the
atmosphere may be charged with aqueous vapour while a deep blue sky is
overhead; and on such occasions the terrestrial radiation would,
notwithstanding the 'clearness,' be intercepted." The great range of the
thermometer is attributable to the absence of that protection against gain
or loss of heat which is afforded when aqueous vapour is present in the
air; and during such weather the rapid abstraction of moisture from the
surface of plants and animals is very deleterious to their healthy
condition. "The nipping of tender plants by frost, even when the air of
the garden is some degrees above the freezing temperature, is also to be
referred to chilling by radiation." Hence the practice of gardeners of
spreading thin mats, of bad radiating material, over tender plants, is
often attended with great benefit.

By means of the process of terrestrial radiation ice is artificially
formed in Bengal, "where the substance is never formed naturally. Shallow
pits are dug, which are partially filled with straw, and on the straw flat
pans containing water which had been boiled is exposed to the clear
firmament. The water is a very powerful radiant, and sends off its heat
into space. The heat thus lost cannot be supplied from the earth--this
source being cut off by the non-conducting straw. Before sunrise a cake of
ice is formed in each vessel.... To produce the ice in abundance, the
atmosphere must not only be clear, but it must be comparatively free from
aqueous vapour."

Considering, therefore, the important consequences attending both
terrestrial and solar radiation, it appears to us that observations from
radiation thermometers are of much more utility in judging of climate than
is usually supposed. These observations are very scanty; and what few are
upon record are not very reliable, principally from bad exposure of the
instruments, while the want of uniformity in construction may be another
cause. Herschell's actinometer and Pouillet's pyrheliometer, instruments
for ascertaining the absolute heating effect of the sun's rays, should,
however, be more generally employed by meteorologists. In comparing
observations on radiation it should be kept in mind, that "the difference
between a thermometer which, properly confined [or shaded], gives the true
temperature of the night air, and one which is permitted to radiate freely
towards space, must be greater at high elevations than at low ones;"[6]
because the higher the place, the less the thickness of the vapour-screen
to intercept the radiation.


=83. Solar Radiation Thermometer.=--"As the interchange of heat between
two bodies by radiation depends upon the relative temperature which they
respectively possess, the earth, by the rays transmitted from the sun
during the day, must be continually gaining an accession of heat, which
would be far from being counterbalanced by the opposite effect of its own
radiation into space. Hence, from sunrise till two or three hours after
mid-day, the earth goes on gradually increasing in temperature, the
augmentation being greatest where the surface consists of materials
calculated, from their colour and texture, to absorb heat, and where it is
deficient in moisture, which, by its evaporation, would have a tendency
to diminish it."[7] It is, therefore, important to have instruments for
measuring the efficacy of solar radiation, apart from those for exhibiting
the temperature of the place in the shade.

[Illustration: Fig. 63.]

Fig. 63 shows the arrangement of Negretti & Zambra's maximum thermometer,
for registering the greatest heat of the sun's direct rays, hence called a
_solar radiation thermometer_. It has a blackened bulb, the scale divided
on its own stem, and the divisions protected by a glass shield. In use it
should be placed nearly horizontally, resting on Y supports of wood or
metal, with its bulb in the full rays of the sun, resting on grass, and,
if possible, so that lateral winds should not strike the bulb; and at a
sufficient distance from any wall, so that it does not receive any
_reflected_ heat from the sun. Some observers place the thermometer as
much as two feet from the ground. It would be very desirable if one
uniform plan could be recognized: that of placing the instrument as
indicated in the figure appears to be most generally adopted, and the
least objectionable.


=84. Vacuum Solar Radiation Thermometer.=--In order that the heat absorbed
by the blackened bulb of the solar radiation thermometer may not in part
be carried off by the currents of air which would come into contact with
it, the instrument has been improved by Messrs. Negretti and Zambra into
the _vacuum solar radiation thermometer_, as illustrated by fig. 64.

[Illustration: Fig. 64.]

This consists of a blackened-bulb radiation thermometer, enclosed in a
glass tube and globe, from which all air is exhausted. Thus protected from
the loss of heat which would ensue if the bulb were exposed, its
indications are from 20 deg. to 30 deg. higher than when placed side by side with
a similar instrument with the bulb exposed to the passing air. At times
when the air has been in rapid motion, the difference between the reading
of a thermometer giving the true temperature of the air in the shade, and
an ordinary solar radiation thermometer, has been 20 deg. only, whilst the
difference between the air temperature and the reading of a radiation
thermometer in vacuo has been as large as 50 deg. It is also found that the
readings are almost identical at distances from the earth varying from six
inches to eighteen inches. By the use of this improvement, it is hoped
that the amounts of solar radiation at different places may be rendered
comparable; hitherto they have not been so; the results found at different
places cannot be compared, as the bulbs of the thermometers are under very
different circumstances as to exposure and currents of air. Important
results are anticipated from this arrangement. The observations at
different places are expected to present more agreement. Observers would
do well to note carefully the effect of any remarkable degree of intensity
in the solar heat upon particular plants, crops, fruit or other trees.


=85. Terrestrial Radiation Thermometer= is an alcohol minimum thermometer,
with the graduations etched upon the stem, and protected by a glass
shield, as shown in figure 65, instead of being mounted on a frame. The
bulb is transparent; that is to say, the spirit is not coloured.

[Illustration: Fig. 65.]

In use, it should be placed with its bulb fully exposed to the sky,
resting on grass, the stem being supported by little forks of wood. The
precautions required with this thermometer are similar to those for
ordinary spirit thermometers, explained at page 76.


[Illustration: Fig. 66.]

=86. AEthrioscope.=--The celebrated experimental philosopher, Sir John
Leslie, was the inventor of this instrument, the purpose of which is to
give a comparative idea of the radiation proceeding from the surface of
the earth towards the sky. It consists, as represented in fig. 66, of two
glass bulbs united by a vertical glass tube, of so fine a bore that a
little coloured liquid is supported in it by its own adhesion, there being
air confined in each of the bulbs. The bulb, _A_, is enclosed in a highly
polished brass sphere, _D_, made in halves and screwed together. The bulb,
_B_, is blackened and placed in the centre of a metallic cup, _C_, which
is well gilt on the inside, and which may be covered by a top, _F_. The
brass coverings defend both bulbs from solar radiation, or any
adventitious source of heat. When the top is on, the liquid remains at
zero of the scale. On removing the top and presenting the instrument to a
clear sky, either by night or by day, the bulb, _B_, is cooled by
terrestrial radiation, while the bulb, _A_, retains the temperature of the
air. The air confined in _B_, therefore, contracts; and the elasticity of
that within _A_ forces the liquid up the tube, to a height proportionate
to the intensity of the radiation. Such is the sensitiveness of the
instrument, that the smallest cloud passing over it checks the rise of the
liquid. Sir John Leslie says:--"Under a clear blue sky, the _aethrioscope_
will sometimes indicate a cold of fifty millesimal degrees; yet, on other
days, _when the air seems equally bright_, the effect is hardly 30 deg." This
anomaly, according to Dr. Tyndall, is simply due to the difference in the
quantity of aqueous vapour present in the atmosphere. The presence of
invisible vapour intercepts the radiation from the aethrioscope, while its
absence opens a door for the escape of this radiation into space.


=87. Pouillet's Pyrheliometer.=--"This instrument is composed of a shallow
cylinder of steel, _A_, fig. 67, which is filled with mercury. Into the
cylinder a thermometer, _D_, is introduced, the stem of which is protected
by a piece of brass tubing. We thus obtain the temperature of the mercury.
The flat end of the cylinder is to be turned towards the sun, and the
surface, _B_, thus presented is coated with lamp black. There is a collar
and screw, _C_, by means of which the instrument may be attached to a
stake driven into the ground, or into the snow, if the observations are
made at considerable heights. It is necessary that the surface which
receives the sun's rays should be perpendicular to the rays; and this is
secured by appending to the brass tube which shields the stem of the
thermometer, a disk, _E_, of precisely the same diameter as the steel
cylinder. When the shadow of the cylinder accurately covers the disk, we
are sure that the rays fall, as perpendiculars, on the upturned surface of
the cylinder.

[Illustration: Fig. 67.]

"The observations are made in the following manner:--First, the instrument
is permitted, not to receive the sun's rays, but to radiate its own heat
for five minutes against an unclouded part of the firmament; the decrease
of the temperature of the mercury consequent on this radiation is then
noted. Next, the instrument is turned towards the sun, so that the solar
rays fall perpendicularly upon it for five minutes; the augmentation of
heat is now noted. Finally, the instrument is turned again towards the
firmament, away from the sun, and allowed to radiate for another five
minutes, the sinking of the thermometer being noted as before. In order to
obtain the whole heating power of the sun, we must add to his observed
heating power the quantity lost during the time of exposure, and this
quantity is the mean of the first and last observations. Supposing the
letter _R_ to represent the augmentation of temperature by five minutes'
exposure to the sun, and that _t_ and _t^1_ represent the reductions of
temperature observed before and after, then the whole force of the sun,
which we may call _T_, would be thus expressed:--_T = R + 1/2(t + t^1)_.

"The surface on which the sun's rays here fall is known; the quantity of
mercury within the cylinder is also known; hence we can express the effect
of the sun's heat upon a given area, by stating that it is competent, in
five minutes, to raise so much mercury so many degrees in
temperature."--_Dr. Tyndall's "Heat considered as a Mode of Motion."_


[Illustration: Fig. 68.]

=88. Sir John Herschell's Actinometer=, for ascertaining the absolute
heating effect of the solar rays, in which _time_ is considered one of the
elements of observation, is illustrated by fig. 68. The actinometer
consists of a large cylindrical thermometer bulb, with a scale
considerably lengthened, so that minute changes may be easily seen. The
bulb is of transparent glass filled with a deep blue liquid, which is
expanded when the rays of the sun fall direct on the bulb. To take an
observation, the actinometer is placed in the shade for one minute and
read off; it is then exposed for one minute to sunshine, and its
indication recorded; it is finally restored to the shade, and its reading
noted. The mean of the two readings in the shade, subtracted from that in
the sun, gives the actual amount of expansion of the liquid produced by
the sun's rays in one minute of time. For further information, see _Report
of the Royal Society on Physics and Meteorology_; or _Kaemtz's
Meteorology_, translated by C. V. Walker; or the _Admiralty Manual of
Scientific Instructions_.




CHAPTER IX.

DEEP-SEA THERMOMETERS.


=89. On Sixe's Principle.=--Thermometers for ascertaining the temperature
of the sea at various depths are constructed to register either the
maximum or minimum temperature, or both. The principle of each instrument
is that of Sixe. There are very few parts of the ocean in which the
temperature below is greater than at the surface, except in the Polar
Seas, where it is generally found to be a few degrees warmer at
considerable depths than at the surface. When the instrument is required
to register only one temperature, it can be made narrower and more
compact--a great advantage in sounding; and with less length of bulb and
glass tube, so that the liability of error is diminished. Hence, the
minimum is the most generally useful for deep-sea soundings. These
thermometers must be sufficiently strong to withstand the pressure of the
ocean at two or three miles of depth, where there may be a force exerted
to compress them exceeding three or four hundred atmospheres (of 15 lbs.
to the square inch).

Many have been the contrivances for obtaining correct deep-sea
indications. Thermometers and machines of various sorts have been
suggested, adopted, and eventually abandoned as only approximate
instruments. The principal reason for such instruments failing to give
correct or reliable indications, has been that the weight or pressure on
the bulbs at great depths has interfered with the correct reading of the
instruments. Thermometers have been enclosed in strong water-tight cases
to resist the pressure; but this contrivance has only had the tendency to
retard the action, so much so as to throw a doubt on the indications
obtained by the instrument so constructed.

The thermometers constructed by Messrs. Negretti and Zambra for this
purpose do not differ materially from those usually made under the
denomination of Sixe's thermometers, except in the following most
important particular:--The usual Sixe's thermometers have a central
reservoir or cylinder containing alcohol; this reservoir, which is the
only portion of the instrument likely to be affected by pressure, has
been, in Negretti and Zambra's new instrument, superseded by a strong
outer cylinder of glass, containing mercury and rarefied air; by this
means the portion of the instrument susceptible of compression, has been
so strengthened that no amount of pressure can possibly make the
instrument vary. This instrument has been tested in every possible manner,
and the results have been highly satisfactory, so much so as to place
their reliability beyond any possible doubt.

The scales are made of porcelain, and are firmly secured to a back of oak,
which holds in a recess the bulb with its protecting shield, and is
rounded off so as to fit easily and firmly in a stout cylindrical copper
case, in which the thermometer is sent down when sounding (see fig. 69).
The lid of the case is made to fit down closely, and water-tight. At the
bottom of the case is a valve opening upward; and the lid has a similar
valve. These allow the water to pass through the case as the instrument
sinks, so that the least amount of obstruction is offered to the descent.
At the lower end of the case is a stout brass spring, to protect the
instrument from a sudden jar if it should touch the bottom while
descending rapidly. As the instrument is drawn up, the valves close with
the weight of water upon them, and it arrives at the surface filled with
water brought up from its lowest position. The deep-sea thermometers used
in the Royal Navy are of this pattern.

[Illustration: Fig. 69.]


=90. Johnson's Metallic Deep-Sea Thermometer.=--The objection to the
employment of mercurial thermometers for ascertaining the temperature of
the ocean at depths, arising from the compression of the bulbs, which was
of such serious consequence previous to the modification made in the
construction of the instrument by Messrs. Negretti and Zambra, led to the
construction of a metallic thermometer altogether free from liability of
disturbance from compression by the surrounding water; which, however, is
certainly not so sensitive to changes of temperature as mercury. This
instrument is the invention of Henry Johnson, Esq., F.R.A.S., and is thus
described by him:--

"During the year 1844 some experiments were made by James Glaisher, Esq.,
F.R.S., on the temperature of the water of the Thames near Greenwich at
the different seasons of the year; when that gentleman found that the
indications of temperature were greatly affected by the pressure on the
bulbs of the thermometers. At a depth of 25 feet this pressure would be
nearly equal to the presence of three-fourths of an atmosphere. These
observations demonstrate the importance of using in deep-sea soundings an
instrument free from liability of disturbance from compression by the
surrounding water, and have ultimately led to the construction of the
thermometer now to be described.

"The instrument is composed of solid metals of considerable specific
gravity, viz. of brass and steel, the specific gravity of these metals
being 8.39 and 7.81 respectively. They are therefore not liable to
compression by the water, which under a pressure of 1,120 atmospheres, or
at a depth of 5,000 fathoms in round numbers, acquires a density or
specific gravity of 1.06. In the construction of this instrument,
advantage has been taken of the well-known difference in the ratios of
expansion and contraction by heat and cold of brass and steel, to form
compound bars of thin bars of these metals riveted together; and which
will be found to assume a slight curve in one direction when heat has
expanded the brass more than the steel, and a slight one in the contrary
direction when cold has contracted the brass more than the steel.

"The indications of the instrument record the motions under changes of
temperature of such compound bars; in which the proportion of brass, the
more dilatable metal, is two-thirds, and of steel one-third.

[Illustration: Fig. 70.]

"Upon one end of a narrow plate of metal about a foot long, _a_, are fixed
three scales of temperature, _h_, which ascend from 25 deg. to 100 deg. F., and
which are shown more clearly in the drawing detached from the instrument.
Upon one of these scales the present temperature is shown by the pointer,
_e_, which turns upon a pivot in its centre. The register index, _g_, to
the maximum temperature, and the index, _f_, to the minimum temperature,
are moved along the other scales by the pin upon the moving pointer, at
_e_, where they are retained by stiff friction. At equal distances from
the centre of the pointer are two connecting pieces, _d d_, by which it is
attached to the free ends of two compound bars, _b b_, and its movements
correspond with the movements of the compound bars under variations of
temperature. The other ends of the bars are fastened by the plate, _c_, to
the plate, _a_, on which the scales of temperature are fixed. The
connection of the bars with both sides of the centre of the pointer
prevents disturbance of indication by lateral concussion. The case of the
instrument has been improved at the suggestion of Admiral FitzRoy, and now
presents to the water a smooth cylindrical surface, with rounded ends, and
without projection of fastenings.

"In surveying expeditions, this instrument would be found useful in giving
notice of variation of depth of water, and of the necessity for taking
soundings. A diminution of the temperature of water has been observed by
scientific voyagers to accompany diminution of depth, as on nearing land,
or approaching hidden rocks or shoals. Attention would also thus be
attracted to the vicinity of icebergs."

This thermometer might easily be modified to serve for several other
important purposes, such as the determination of the temperature of
intermittent hot springs, and mud volcanoes.

[Illustration: Fig. 71.]

The principle of this thermometer is not altogether new; but the duplicate
arrangement of the bars, which effectually prevents the movement of the
indices by any shaking, and the application are certainly novel. Professor
Trail, in the _Library of Useful Knowledge_, writes:--"In 1803, Mr. James
Crighton, of Glasgow, published a new 'metallic thermometer,' in which
the unequal expansion of zinc and iron is the moving power. A bar is
formed by uniting a plate of zinc (fig. 71), _c d_, 8 inches long, 1 inch
broad, and 1/4 inch thick, to a plate of iron, _a b_, of the same length.
The lower extremity of the compound bar is firmly attached to a mahogany
board at _e e_; a pin, _f_, fixed to its upper end, plays in the forked
opening in the short arm of the index, _g_. When the temperature is
raised, the superior expansion of the zinc, _c d_, will bend the whole
bar, as in the figure; and the index, _g_, will move along the graduated
arc, from right to left, in proportion to the temperature. In order to
convert it into a _register thermometer_, Crighton applied two slender
hands, _h h_, on the axis of the index; these lie below the index, and are
pushed in opposite directions by the stud, _i_,--a contrivance seemingly
borrowed from the instrument of Fitzgerald," a complicated metallic
thermometer, described by the Professor previously.




CHAPTER X.

BOILING-POINT THERMOMETERS.


=91. Ebullition.=--The temperature at which a fluid _boils_ is called the
_boiling-point_ of that particular fluid. It is different for different
liquids; and, moreover, in the same liquid it varies with certain changes
of circumstance. Thus the same liquid in various states of purity would
have its boiling temperature altered in a slight degree. There is also an
intimate connection with the pressure under which a fluid is boiled, and
its temperature of ebullition. Liquids boiled in the open air are
subjected to the atmospheric pressure, which is well known to vary at
different times and places; and the boiling-point of the liquid exhibits
corresponding changes. When the pressure is increased on the surface of
any fluid, the temperature of ebullition rises; and with a decrease of
pressure, the boiling goes on at a lower degree of heat.

In the case of water, we commonly state the boiling-point to be 212 deg. F.;
but it is only so at the level of the sea, under the mean pressure of the
atmosphere, represented, in the latitude of London, by a column of 29.905
inches of mercury, at a temperature of 32 deg. F., and when the water is fresh
and does not contain any matter chemically dissolved in it. When steam is
generated and confined in a boiler, the pressure upon the boiling water
may be several times greater than that of the atmosphere. Experimentally
it has been found, that if the pressure in the boiler be 25 lbs. on the
square inch, the temperature of the boiling water, and of the steam
likewise, is raised to 241 deg.; while under the exhausted receiver of an
air-pump, water will boil at 185 deg., when the pressure is reduced to 17
inches of mercury.


=92. Relation between the Boiling-Point and Elevation.=--Now, as the
atmospheric pressure is diminished by ascent, as shown by the fall of
mercury in the barometer, it follows that in elevated localities water, or
any other fluid, heated in the open air, will boil at a temperature lower
than at the sea-level. Therefore, there must be some relation between the
height of a hill, or mountain, and the temperature at which a fluid will
boil at that height. Hence, the thermometer, as used to determine the
boiling-point of fluids, is also an indicator of the atmospheric pressure;
and may be used as a substitute for the barometer in measuring elevations.

If the atmospheric pressure were constant at the sea-level, and always the
same for definite heights, we might expect the boiling-points of fluids
also to be in exact accordance with height; and the relation once
ascertained, we could readily, by means of the thermometer and boiling
water, determine an unknown height, or for a known elevation assert the
boiling temperature of a liquid. However, as the atmospheric pressure is
perpetually varying at the same place, within certain limits, so there
are, as it were, sympathetic changes in the boiling temperatures of
fluids. It follows from this, that heights can never be accurately
measured, either by the barometer or the boiling-point thermometer, by
simply observing at the places whose elevations are required. To determine
a height with any approach to accuracy, it is necessary that a similar
observation should be made at the same time at a lower station, not very
remote laterally from the upper, and that they should be many times
repeated. When such observations have been very carefully conducted, the
height of the upper station above the lower may be ascertained with great
precision, as has been repeatedly verified by subsequent trigonometrical
measurement of elevations so determined. If the lower station be at the
sea-level, of course the absolute height of the upper is at once obtained.


=93. Mountain Thermometer; sometimes called Hypsometric Apparatus.=--We
have now to examine the construction of the boiling-point thermometer, and
its necessary appendages, as adapted for the determination of heights.

Messrs. Negretti and Zambra's arrangement of the instrument is shown in
figures 72 and 73.

[Illustration: Fig. 72.]

[Illustration: Fig. 73.]

The thermometer is made with an elongated bulb, so as to be as sensitive
as possible. The scale, about a foot long, is graduated on the stem, and
ranges from 180 deg. to 214 deg., each degree being sufficiently large to show the
divisions of tenths of a degree. A sliding metallic vernier might perhaps
with advantage be attached to the stem, which would enable the observer to
mark hundredths of a degree; which, however, he can pretty well do by
estimation. The boiler is so contrived as to allow, not only the bulb, but
the stem also of the thermometer, to be surrounded by the steam. The
arrangement is readily understood by reference to the accompanying
diagram, fig. 73.

_C_, is a copper boiler, supported by a tripod stand so as to allow a
spirit-lamp, _A_, made of metal to be placed underneath. The flame from
the lamp may be surrounded by a fine wire gauze, _B_, which will prevent
it being extinguished when experimenting in the external air. _E E E_, is
a three-drawn telescope tube, proceeding from the boiler, and open also at
top. Another tube, similarly constructed, envelops this, as shown by _D D
D_. This tube is screwed to the top of the boiler, and has two openings,
one at the top to admit the thermometer, the other low down, _G_, to give
vent to the steam. As the steam is generated, it rises in the inner tube,
passes down between the tubes, and flows away at _G_. The thermometer is
passed down, supported by an india-rubber washer, fitting steam tight, so
as to leave the top of the mercury, when the boiling-point is attained,
sufficiently visible to make the observation. The telescopic movement, and
the mode of supporting the thermometer, enable the observer always to keep
the bulb near the water, and the double tube gives all the protection
required to obtain a steady boiling-point. Some boiling-point thermometers
are constructed with their scales altogether exposed to the air, which may
be very cold, and consequently may contract to some extent the thread of
mercury outside the boiler. The steam, having the same temperature as the
boiling water, keeps the tube, throughout nearly its whole length, at the
same degree of heat, in the apparatus described. The whole can be packed
in a tin case very compactly and securely for travelling, as in fig. 72.

_Directions for Using._--When the apparatus is required for practical use,
sufficient water must be poured into the boiler to fill it about one
third, through an opening, _F_, which must be afterwards closed by the
screw plug. Then apply the lighted lamp. In a short time steam will issue
from _G_; and the mercury in the thermometer, kept carefully immersed,
will rise rapidly until it attains a stationary point, which is the
boiling temperature. The observation should now be taken and recorded with
as much accuracy as possible, and the temperature of the external air must
be noted at the same time by an ordinary thermometer.

The water employed should be pure. Distilled water would therefore be the
best. If a substance is held mechanically suspended in water, it will not
affect the boiling-point. Thus, muddy water would serve equally as well as
distilled water. However, as it cannot be readily ascertained that nothing
is dissolved chemically when water is dirty, we are only correct when we
employ pure water.


=94. Precautions to ensure correct Graduation.=--Those who possess a
boiling-point thermometer should satisfy themselves that it has been
correctly graduated. To do this, it is advisable to verify it with the
reading of a standard barometer reduced to 32 deg. F. The table of "Vapour
Tension" (given at p. 62) will furnish the means of comparison. Thus, if
the reduced reading of the barometer, corrected also for latitude, be
29.922, the thermometer should show 212 deg. as the boiling-point of water at
the same time and place; if 29.745, the thermometer should read 211.7; and
so on as per table. In this way the error of the chief point of the scale
can be obtained. Other parts of the scale may be checked with a standard
thermometer, by subjecting both to the same temperature, and comparing
their indications. The graduations as fixed by some makers are not always
to be trusted; and this essential test should be conducted with the utmost
nicety and care.

Admiral FitzRoy writes, in his _Notes on Meteorology_:--"Each degree of
the boiling-point thermometer is equivalent to about 550 _feet of ascent_,
or one-tenth to 55 feet; therefore, the smallest error in the graduation
of the thermometer itself will affect the height deduced materially.

"In the thermometer which is graduated from 212 deg. (the boiling-point) to
180 deg., similarly to those intended for the purpose of measuring heights,
there must have been a starting point, or zero, from which to begin the
graduation. I have asked an optician in London how he fixed that zero, the
boiling-point. 'By boiling water at my house,' he replied. 'Where is your
house?' In such a part of the town, he answered. I said: 'What height is
it above the sea?' to which he replied, 'I do not know;' and when I asked
the state of the barometer when he boiled the water, whether the mercury
was high or low, he said that he had not looked at it! Now, as this
instrument is intended to measure heights and to decide differences of
some hundred, if not thousand feet upwards, at least one should endeavour
to ascertain a reliable starting point. From inquiries made, I believe
that the determination of the boiling-point of ordinary thermometers has
been very vague, not only from the extreme difficulties of the process
itself (which are well known to opticians), but from the radical errors of
not allowing for the pressure of the atmosphere at the time of
graduation--which may be much, even an inch higher or lower, than the
mean, or any _given height_--while the elevation of the place above the
level of the sea is also unnoticed. Then there is another source of error,
a minor one, perhaps: the inner limit, the 180 deg. point, is fixed only by
comparison with another thermometer; it may be right, or it may be very
much out, as may be the intermediate divisions; for the difficulty of
ascertaining degree by degree is great: and it must be remembered that the
measurement of a very high mountain depends upon those inner degrees from
200 deg. down to 180 deg., thereabouts. Hence, the difficulty of making a reliable
observation by boiling water seems to be greater than has been generally
admitted."


=95. Method of Calculating Heights from Observations with the Mountain
Thermometer.=--Having considered how to make observations with the proper
care and accuracy, it becomes necessary to know how to deduce the height
by calculation. That a constant intimate relation exists between the
boiling temperature of water and the pressure of the air, we have already
learned. This knowledge is the result of elaborate experiments made by
several scientific experimentalists, who have likewise constructed formulae
and tables for the conversion of the boiling temperatures into the
corresponding pressures of vapour, or, which is equivalent, of the
atmosphere, when the operation is performed in the open air. As might be
expected, there is not a perfect accord in the results arrived at by
different persons. Regnault is the most recent, and his experiments are
considered the most reliable.

From Regnault's table of vapour tension, we can obtain the pressure in
inches of mercury at 32 deg., which corresponds to the observed boiling-point;
or _vice versa_, if required. From the pressure, the height may be deduced
by the method for finding heights by means of the barometer.

The following table expresses very nearly the elevation in feet
corresponding to a fall of 1 deg. in the temperature of boiling water:--

  Boiling Temperatures      Elevation in Feet
      between.               for each Degree.

  214 deg. and 210--                  520
  210  and 200--                  530
  200  and 190                    550
  190  and 180                    570

These numbers agree very well with the results of theory and actual
observation. The assumption is that the boiling-point will be diminished
1 deg. for each 520 feet of ascent until the temperature becomes 210 deg., then
530 feet of elevation will lower it one degree until the water boils at
200 deg., and so on; the air being at 32 deg.

Let _H_ represent the vertical height in feet between two stations; _B_
and _b_, the boiling-points of water at the lower and upper stations
respectively; _f_, the factor found in the above table. Then

  _H_ = _f_(_B_ - _b_)

Further, let _m_ be the mean temperature of the stratum of air between the
stations. Now, if the mean temperature is less than 32 deg., the column of air
will be shorter; and if greater, longer than at 32 deg. According to
Regnault, air expands 1/491.13 or .002036 of its volume at 32 deg., for each
degree increase of heat. Calling the correction due to the mean
temperature of air _C_, its value will be found from the equation,

  _C_ = _H_ (_m_ - 32) .002036

Calling the corrected height _H'_, it will be found from the formula,

            _H'_ = _H_ + _H_ (_m_ - 32) .002036
  that is,  _H'_ = _H_ { 1 + (_m_ - 32) .002036 }

and substituting the value of _H_,

  _H'_ = _f_(_B_ - _b_) { 1 + (_m_ - 32) .002036 }

Strictly, according to theoretical considerations, there is a correction
due to latitude, as in the determination of heights by the barometer; but
its value is so small that it is practically of no importance.

If a barometer be observed at one of the stations, the table of vapour
tensions (p. 62) will be useful in converting the pressure into the
corresponding boiling-point, or _vice versa_; so that the difference of
height may be found either by the methods employed for the boiling-point
thermometer or the barometer.

In conclusion, it may be remarked that observers who have good instruments
at considerable elevations, as sites on mountains or plateaus, would
confer a benefit to science, by registering for a length of time the
barometer along with the boiling temperature of water, as accurately as
possible. Such observations would serve to verify the accuracy of
theoretical deductions, and fix with certainty the theoretical scale with
the barometer indications.

_Example, in calculating Heights from the Observations of the
Boiling-point of Water._--1. At Geneva the observed boiling-point of water
was 209 deg.335; on the Great St. Bernard it was 197 deg.64; the mean
temperature of the intermediate air was 63 deg.5; required the height of the
Great St. Bernard above Geneva.

Method by formula:--

  _H'_ = _f_ (_B_ - _b_) { 1 + (_m_ - 32 deg.) .002036 }

In this case _f_ is between 530 and 550, or 540.

  _B_ = 209.335          _m_ = 63.5
  _b_ = 197.64                 32
        -------                -----
         11.695                31.5
  _f_  =    540                  .002036
        -------                ---------
         6315.3                 0.0641340
          1.064                 1
        -------                 -----
  _H'_ = 6719.5 feet.           1.064
         ======

Method by Tables supplied with boiling-point apparatus made by Messrs.
Negretti and Zambra:--

  209.335 gives 1464 in Table I.
  197.64      "     7736      "
                    ----
                    6272
   63.5       "        1.07 in Table II.
                    ----
  Height            6711
                    ====


=96. Thermometers for Engineers.=--_1st. Salinometer._--Under the
circumstances at which fresh water boils at 212 deg., sea water boils at
213 deg.2. The boiling temperature is raised by the chemical solution of any
substance in the water, and the more with the increase of matter
dissolved.

From a knowledge of this principle, marine engineers make use of the
thermometer to determine the amount of salts held in solution by the water
in the boilers of sea-going steamers. Common sea-water contains 1/33 of
its volume of salt and other earthy matters. As evaporation proceeds, the
solution becomes proportionally stronger, and more heat is required to
produce steam. The following table from the work of Messrs. Main and
Brown, on the Marine Steam-Engine, shows the relation between the
boiling-point under the mean pressure of the atmosphere, or 80 inches of
mercury, and the proportion of matter dissolved in the water:--

  Proportion of Salt in 100 parts of water   0    Boiling-point 212 deg.
            "                     "         1/33       "        213.2
            "                     "         2/33       "        214.4
            "                     "         3/33       "        215.5
            "                     "         4/33       "        216.6
            "                     "         5/33       "        217.9
            "                     "         6/33       "        219.0
            "                     "         7/33       "        220.2
            "                     "         8/33       "        221.4
            "                     "         9/33       "        222.5
            "                     "        10/33       "        223.7
            "                     "        11/33       "        224.9
            "                     "        12/33       "        226.0

When the salts in solution amount to 12/33, the water is saturated. It has
also been ascertained that, when a solution of 4/33 is attained,
incrustation of the substances commences on the boiler. Hence, it is a
rule with engineers to expel some of the boiling water, when the
thermometer indicates a temperature of 216 deg., and introduce some more cold
water, in order to prevent incrustation, which not only injures the
boiler, but opposes the passage of heat to the water. The thermometer used
for this purpose should be very accurately graduated, and the scale must
be considerably higher than, though it need not read much below 212 deg.

_2nd. Pressure Gauge._--The elasticity of gases augments by increase of
temperature, and _vice versa_; it follows, therefore, that when steam is
generated in a closed boiler, its temperature rises beyond the boiling
temperature of 212 deg., owing to the increased pressure upon the water. The
law connecting the pressure and the corresponding temperature of steam is
the same as that upon which the boiling of fluids under diminished
atmospheric pressure takes place. Hence, the indications of the
thermometer become exponents of steam pressure. Engineers are furnished,
in works on the steam-engine, with tables, from which the pressure
corresponding to a given temperature, or the converse, can be obtained by
mere inspection.

[Illustration: Fig. 74.]

Fig. 74 represents the thermometer employed as a steam-pressure gauge. It
is fitted in a brass case, with screw-plug and washers for closing the
boiler when the thermometer is not in use. The scale shows the pressure
corresponding to the temperature, from 15 to 120 lbs., above the
atmospheric pressure, which is usually taken as 15 lbs. on the square
inch.




CHAPTER XI.

INSTRUMENTS FOR ASCERTAINING THE HUMIDITY OF THE AIR.


=97. Hygrometric Substances.=--The instruments devised for the purpose of
ascertaining the humidity of the atmosphere are termed _hygrometers_. The
earliest invented hygrometers were constructed of substances readily acted
upon by the vapour in the air, such as hair, grass, seaweed, catgut, &c.,
which all absorb moisture, and thereby increase in length, and when
deprived of it by drying they contract. Toy-like hygrometers, upon the
principle of absorption, are still common as ornaments for mantel-pieces.
A useful little instrument of this class, formed from the beard of the
wild oat, is made to resemble a watch in external appearance, and is
designed to prove the dampness or dryness of beds: a moveable hand points
out on the dial the hygrometric condition of the clothes upon which the
instrument is laid.


=98. Saussure's Hygrometer=, formerly used as a meteorologic instrument,
but now regarded as an ornamental curiosity, is represented in fig. 75.
Its action depends upon a prepared hair, fixed at one end to the frame of
the instrument, and wound round a pulley at the other. The pulley carries
a pointer which has a counterpoise sufficient to keep the hair stretched.
By this means the shrinking and lengthening of the hair cause the pointer
to traverse a graduated arc indicating the relative humidity.

[Illustration: Fig. 75.]

Such instruments, however ingenious, are not of scientific value; because
they do not admit of rigid comparison, are liable to alter in their
contractile and expansive properties, and cannot be made to indicate
precisely alike.


=99. Dew-Point.=--The amount of water which the air can sustain in an
invisible form increases with the temperature; but for every definite
temperature there is a limit to the amount of vapour which can be thus
diffused. When the air is cooled, the vapour present may be more than it
can sustain; part will then be condensed as dew, rain, hail or snow,
according to the meteorologic circumstances. The temperature which the air
has when it is so fully saturated with vapour that any excess will be
deposited as dew, is called the _dew-point_.


=100. Drosometer.=--"To measure the quantity of dew deposited each night,
an instrument is used called a _Drosometer_. The most simple process
consists in exposing to the open air bodies whose exact weight is known,
and then weighing them afresh after they are covered with dew. According
to Wells, locks of wool, weighing about eight grains, are to be preferred,
which are to be divided [formed] into spherical masses of the diameter of
about two inches."--_Koemtz._


=101. Humidity.=--The proportion existing between the amount of vapour
actually present in the air at any time, and the quantity necessary to
completely saturate it, is called _the degree of humidity_. It is usually
expressed in a centesimal scale, 0 being perfect dryness, and 100 complete
saturation.

The pressure, or tension, of vapour at the dew-point temperature, divided
by the tension of vapour at the air temperature and the quotient
multiplied by 100, gives the degree of humidity. (Regnault's Tables should
be used.)

Hence the utility of instruments for determining the dew-point.


=102. Leslie's Hygrometer.=--This instrument consists of a glass syphon
tube, terminated with a bulb or ball at each end, turned outwards from
each other, as in fig. 76. The tube is partly filled with concentrated
sulphuric acid, tinged by carmine. One of the balls is covered smoothly
with fine muslin, and is kept continually moistened with pure water, drawn
from a vase placed near it by the capillary attraction of a few strands of
clean cotton-wick. The descent of the coloured liquid in the other stem
will mark the diminution of temperature caused by the evaporation of the
water from the humid surface. The drier the ambient air is, the more
rapidly will the evaporation go on; and the cold produced will be greater.
When the air is nearly saturated with moisture, the evaporation goes on
slowly; the cold produced is moderate, because the ball regains a large
portion of its lost heat from surrounding bodies; and the degree of
refrigeration of the ball is an index of the dryness of the air.

[Illustration: Fig. 76.]

"Should the water become frozen on the ball, this hygrometer will still
act; for evaporation goes on from the surface of ice in proportion to the
dryness of the air. Leslie estimates, that when the ball is moist, air, at
the temperature of the ball, will take up moisture equal to the
sixteen-thousandth part of its weight, for each degree of his hygrometer;
and as ice in melting requires one-seventh of the caloric consumed in
converting water into vapour, when the ball is frozen, the hygrometer will
sink more than when wet by 1 deg. in 7 deg.; and hence, in the frozen state, we
must increase the value of the degrees one-seventh: so that each of them
will correspond to an absorption of moisture equal to
one-fourteen-thousandth part of the weight of the air.

"When this hygrometer stands at 15 deg., the air feels damp; from 30 deg. to 40 deg.,
we reckon it dry; from 50 deg. to 60 deg., very dry; and from 70 deg. upwards, we
should call it intensely dry. A room would feel uncomfortable, and would
probably be unwholesome, if the instrument in it did not reach 30 deg.[8] In
thick fogs it keeps almost at the beginning of the scale. In winter, in
our climate, it ranges from 5 deg. to 15 deg.; in summer often from 15 deg. to 55 deg.;
and sometimes attains 80 deg. or 90 deg. The greatest degree of dryness ever
noticed by Leslie was at Paris, in the month of September, when the
hygrometer indicated 120 deg."--_Professor Trail, in "Library of Useful
Knowledge."_

In estimating the value of the indications of this hygrometer, it should
be borne in mind that the scale adopted by Leslie was _millesimal_, that
is to say, from the freezing to the boiling-point of water was divided
into a thousand parts; ten millesimal degrees are therefore equal to one
of the scale of Celsius.


103. DANIEL'S HYGROMETER.

This instrument was invented about the year 1820, by Professor Daniel, the
distinguished author of _Meteorological Essays_; and it entirely
superseded all hygrometers depending upon the absorption of moisture. The
form of the instrument is shown in fig. 77.

[Illustration: Fig. 77.]

It consists of a glass tube, about one-eighth of an inch in diameter of
bore, bent twice at right angles, and terminated, at each end, in a bulb
about one inch and a quarter in diameter. In one limb of the tube is
enclosed a delicate thermometer, which descends to the centre of the
adjoining bulb, which is about three-parts filled with sulphuric ether.
All the other parts of the tube are carefully freed from air, so that they
are occupied by the vapour of the ether. This bulb is generally made of
black glass; the other is transparent, but covered with a piece of fine
muslin. The support for the tube has a thermometer attached, which shows
the temperature of the external air. The tube can be removed from the
stand, and the parts are made to pack, with a necessary phial of ether, in
a small box, which can easily be got into the pocket.

_How to use the Hygrometer._--This instrument gives the dew-point by
direct observation, which must be made in the following manner:--Having
fixed the tube upon the stand, with the bulbs vertically downward, the
ether is all caused to flow into the lower ball by inclining the tube. The
temperature of the air is noted by the exposed thermometer. Then some
ether is poured, from a dropping tube fitting into the neck of the phial,
upon the muslin-covered bulb. The rapid evaporation of this ether cools
the bulb and causes condensation of the ethereal vapour in its interior.
This gives rise to rapid evaporation of the ether in the lower bulb,
whereby its temperature is greatly reduced. The air in the vicinity is
deprived of its warmth by the cold bulb, and is soon cooled to the
temperature at which it is perfectly saturated with the vapour which it
contains. Cooled ever so little below this temperature, some aqueous
vapour will be condensed, and will form a dew upon the black-glass bulb.
At the first indication of the deposit of dew the reading of the internal
thermometer is taken: which is the dew-point.

This hygrometer has undeniable disadvantages. The surface upon which the
dew condenses is small, and requires a peculiar direction of light in
which to see it well. The observer, having his attention on the bulb and
the thermometer, cannot always fix with precision the dew-point; and hence
he is recommended to note the temperature at the appearance and at the
disappearance of the dew, in order that the chance of error may be
diminished. Without doubt, the necessarily long continuance of the
observer near the instrument influences, to some extent, the observed
temperatures; and the difficulty of not being always able to procure pure
ether for the experiments is not the least of the drawbacks to the use of
the instrument. Some of these disadvantages are obviated in Regnault's
hygrometer.


104. REGNAULT'S CONDENSER HYGROMETER

(Fig. 78) consists of a tube, _C_, made of silver, very thin, and
perfectly polished; the tube is larger at one end than the other, the
large part being 1.8 inches in depth, by 0.8 in diameter; this is fitted
tightly to a brass stand, _B_, with a telescopic arrangement for adjusting
when making an observation.

[Illustration: Fig. 78.]

The tube, _C_, has a small lateral tubulure, to which is attached an
India-rubber tube, with ivory mouth-piece; this tubulure enters _C_ at
right angles near the top, and traverses it to the bottom of the largest
part.

A delicate thermometer, _D_, is inserted through a cork, or India-rubber
washer, at the open end of the tube, _C_, the bulb of which descends to
the centre of its largest part.

_G_ is an attached thermometer for taking the temperature of the air, and
_F_ is a bottle containing ether.

_To use the Condenser Hygrometer_, a sufficient quantity of ether is
poured into the silver tube to cover the thermometer bulb: on allowing air
to pass bubble by bubble through the ether, by breathing in the tube, _E_,
an uniform temperature will be obtained; if the ether continues to be
agitated, by breathing briskly through the tube a rapid reduction of
temperature will be the result; at the moment the ether is cooled down to
the dew-point temperature, the external surface of that portion of the
silver tube containing ether will become covered with a coating of
moisture, and the degree shown by the thermometer at that instant will be
the temperature of the dew-point.

This form of hygrometer, for ascertaining by direct observation the
dew-point, is so superior to Daniell's, both from its being more certain
in its indications and economical in use, that Messrs. Negretti and
Zambra have been induced to modify it, and reduce its price to little more
than that of a good Daniell's Hygrometer.


=105. Temperature of Evaporation.=--When the air is not saturated with
vapour, evaporation is going on with more or less activity, according as
the temperature is high or low, rising or falling. Now vapour cannot be
formed without an expenditure of heat; as we invariably find that the
process of evaporation lowers the temperature of the liquid from which the
vapour is produced, and, by communication, that of contiguous substances
also. Thus the emigrant, crossing the line under the scorching influence
of the vertical sun, wraps a wet towel round his can of water, swings it
in the breeze, to evaporate the moisture of the towel, and obtains a glass
of cool water. So also, European residents in India, during the hot
season, spread out mats in their apartments, and keep them wet, in order
that the evaporation may cool the air. This principle has been applied,
for the purpose of ascertaining the hygrometric condition of the air, in
the instrument known as Mason's hygrometer, or psychrometer, which is now
in general use, from its simplicity, accuracy, and ease of observing.


106. MASON'S HYGROMETER.

=The Dry and Wet Bulb Hygrometer, or Psychrometer=, known also as Mason's
hygrometer (fig. 79), consists of two parallel thermometers, as nearly
identical as possible, mounted on a wooden bracket, one marked _dry_, the
other _wet_. The bulb of the wet thermometer is covered with thin muslin,
and round the neck is twisted a conducting thread of lamp-wick, which
passes into a vessel of water, placed at such a distance as to allow a
length of conducting thread, of about three inches; the cup or glass is
placed on one side, and a little beneath, so that the water within may not
affect the reading of the _dry bulb thermometer_. In observing, the eye
should be placed on a level with the top of the mercury in the tube, and
the observer should refrain from breathing whilst taking an observation.

[Illustration: Fig. 79.]

The _dry_ bulb thermometer indicates the temperature of the air itself;
while the wet bulb, cooled by evaporation, shows a lower temperature
according to the rapidity of evaporation.

_To find the Dew-point._--From the readings of the two thermometers, the
dew-point can be deduced by formulae (that known as Apjohn's is considered
the most theoretically true), or from the valuable Hygrometric Tables by
J. Glaisher, Esq., F.R.S.

For practical purposes in estimating the comparative humidity, the annexed
table, which is a reduction from Mr. Glaisher's elaborate work, will be
sufficient; it will at least serve to assist in familiarising the
inexperienced in the value of the psychrometer's indications:--

  +------------------------------------------+
  |            | Difference between Dry-bulb |
  |            |    and Wet-bulb Readings.   |
  |Temperature |-----------------------------|
  |   by the   | 2 deg. | 4 deg. | 6 deg. | 8 deg. | 10 deg.| 12 deg.|
  |  Dry Bulb  |-----------------------------|
  |Thermometer.|     Degree of Humidity.     |
  |------------------------------------------|
  |     34 deg.    | 79 | 63 | 50 | .. | .. | .. |
  |     36     | 82 | 66 | 53 | .. | .. | .. |
  |     38     | 83 | 68 | 56 | 45 | .. | .. |
  |     40     | 84 | 70 | 58 | 47 | .. | .. |
  |     42     | 84 | 71 | 59 | 49 | .. | .. |
  |     44     | 85 | 72 | 60 | 50 | .. | .. |
  |     46     | 86 | 73 | 61 | 51 | .. | .. |
  |     48     | 86 | 73 | 62 | 52 | 44 | .. |
  |     50     | 86 | 74 | 63 | 53 | 45 | .. |
  |     52     | 86 | 74 | 64 | 54 | 46 | .. |
  |     54     | 86 | 74 | 64 | 55 | 47 | .. |
  |     56     | 87 | 75 | 65 | 56 | 48 | .. |
  |     58     | 87 | 76 | 66 | 57 | 49 | .. |
  |     60     | 88 | 76 | 66 | 58 | 50 | 43 |
  |     62     | 88 | 77 | 67 | 58 | 50 | 44 |
  |     64     | 88 | 77 | 67 | 59 | 51 | 45 |
  |     66     | 88 | 78 | 68 | 60 | 52 | 45 |
  |     68     | 88 | 78 | 68 | 60 | 52 | 46 |
  |     70     | 88 | 78 | 69 | 61 | 53 | 47 |
  |     72     | 89 | 79 | 69 | 61 | 54 | 48 |
  |     74     | 89 | 79 | 70 | 62 | 55 | 48 |
  |     76     | 89 | 79 | 71 | 63 | 55 | 49 |
  |     78     | 89 | 79 | 71 | 63 | 56 | 50 |
  |     80     | 90 | 80 | 71 | 63 | 56 | 50 |
  |     82     | 90 | 80 | 72 | 64 | 57 | 51 |
  |     84     | 90 | 80 | 72 | 64 | 57 | 51 |
  |     86     | 90 | 80 | 72 | 64 | 58 | 52 |
  +------------------------------------------+

The total quantity of aqueous vapour which at any temperature can be
diffused in the air being represented by 100, the per-centage of vapour
actually present will be found in the table opposite the temperature of
the dry thermometer, and under the difference between the dry-bulb and
wet-bulb temperatures. The degree of humidity for intermediate
temperatures and differences to those given in the table can be easily
estimated sufficiently accurately for most practical purposes.

The difference between the two thermometer readings taken from the reading
of the wet bulb, gives the dew-point very nearly, when the air is at any
temperature between freezing and 80 deg. This simple rule will be found
serviceable to horticulturists, since it will enable them to estimate the
chilling effect of dew or hoar-frost on tender plants.

_Use as an Indicator of Weather._--In our climate, the usual difference
between the thermometer readings,--in the open air, shaded from the sun,
reflected heat, and currents of air,--ranges from one to twelve degrees.
In hot and dry climates, as India and Australia, the range out of doors
has been found as much as 30 deg., occasionally.

When the moisture is frozen, the bulb should be wetted afresh, and the
reading taken just before it again freezes; but the observation then is of
little value, and for general purposes need not be taken, as the air is
known to be dry in frosty weather.

The muslin or cotton rag should be washed once or twice a week by pouring
water over the bulb; and it should be replaced by a fresh piece at least
once a month. Accuracy depends very much upon keeping the wet bulb clean,
and not _too_ wet.

In connection with the barometer, this hygrometer is very useful, not only
on land, but especially at sea, where other kinds of hygrometers cannot be
practically used. A fall in the barometer is indicative of coming wind or
rain: if the hygrometer shows increasing dampness by the difference of the
readings becoming smaller,--rain may therefore be anticipated. On the
contrary, if the hygrometer shows continuing or increasing dryness, a
stronger wind is probable, without rain.

_Domestic Uses._--Mason's hygrometer is useful in regulating the moisture
of the air of apartments; a difference in the thermometer readings of from
5 deg. to 8 deg. being considered healthy. Many complaints require that the
temperature and humidity of the air which the invalid breathes should be
carefully regulated. Hence it is a valuable household instrument. In a
room, it should be placed away from the fire as much as possible, but not
exposed to draughts of air.

Figs. 80 and 81 show cheap arrangements of the instrument for domestic
purposes. Other arrangements are given to the instrument to make it
suitable for exhibiting the hygrometrical state of the air in hot-houses,
conservatories, malting-houses, warehouses, manufactories, &c.

[Illustration: Fig. 80.]

[Illustration: Fig. 81.]

[Illustration: Fig. 82.]

Fig. 82 shows the instrument arranged on brass tripod stand, with folding
legs and metal cover, to render it portable.


=107. Self-Registering Hygrometer.=--A maximum thermometer and a minimum
thermometer, each fitted up as a wet-bulb thermometer, record the highest
and lowest temperature of evaporation during the interval of observation.
Negretti's mercurial maximum, and an alcohol minimum, answer best.


=108. Causes of Dew.=--"The aqueous vapour of our atmosphere is a powerful
radiant; but it is diffused through air which usually exceeds its own mass
more than one hundred times. Not only, then, its own heat, but the heat of
the large quantity of air which surrounds it, must be discharged by the
vapour, before it can sink to its point of condensation. The retardation
of chilling due to this cause enables good solid radiators, at the earth's
surface, to outstrip the vapour in their speed of refrigeration; and
hence, upon these bodies, aqueous vapour may be condensed to liquid, or
even congealed to hoar-frost, while at a few feet above the surface it
still maintains its gaseous state."[9] The amount of moisture so deposited
will vary with different atmospheric conditions. If the sky be decidedly
cloudy or misty, the heat radiated from the earth will be partly restored
by counter-radiation from the visible vapour; the cooling of the earth's
surface will, therefore, take place slowly, and little dew will be
deposited. On the other hand, if the air contain transparent vapour, and
the sky appear clear, the counter-radiation will be less, the earth will
cool rapidly, and the deposit of dew will be copious; provided the night
be comparatively calm, for, when the wind blows, the circulating air
supplies heat to the radiating substances, and prevents any considerable
chilling.

The dew which falls in tropical countries greatly exceeds in abundance
what we experience in our climate; because the air is there, from the
great heat, capable of sustaining a large amount of vapour in the
transparent state, and the conditions most favourable for a maximum
reduction of temperature by radiation are present. At those places, or
upon those substances which cool the lowest and most readily, the dew
falls most copiously.


[Illustration: Fig. 83.]

=109. Plan of Exposing Thermometers=, &c.--Figure 83 is an illustration of
a convenient slab for supporting thermometers in an exposed position
attached to a stand (such as Glaisher's, described in Chapter XVI.) for
ordinary scientific observations. It has a projecting ledge, _B_, to carry
off rain from the instruments, the slab, _A_, being erected vertically.
The hygrometer is placed at _E_, with the vase of water at _F_. An alcohol
minimum thermometer is represented at _C_, in the position most favourable
to its certain action; and at _D_ is shown one of Negretti & Zambra's
maximum thermometers, the position of which may be more nearly horizontal
than there exhibited, although a slight depression of the bulb-end of the
frame is desirable, but not necessary, as this thermometer can be used in
any position.




CHAPTER XII.

INSTRUMENTS USED FOR MEASURING THE RAINFALL.


The instruments in use for measuring the quantity of rain which falls on a
given spot are of very simple construction. Perhaps the simplest is:--


=110. Howard's Rain-Gauge.=--It consists of a copper funnel, a stout glass
or stone bottle, and a measuring glass. The bottle is to be placed upon
the ground, with the funnel resting on its neck. A brass band or cylinder
fixed upon the outer surface of the funnel envelops the neck of the
bottle, and the pipe of the funnel extends nearly to the bottom of the
bottle; so that loss by evaporation is avoided as much as possible. The
receiving space of the funnel is formed by a brass ring, five inches in
diameter, very accurately turned. The measuring vessel enables the
observer to note the rainfall in inches, tenths, and hundredths of an
inch.


[Illustration: Fig. 84.]

=111. Glaisher's Rain-Gauge.=--The rain-gauge designed by Mr. Glaisher,
the well-known meteorologist, and used by most observers of the present
day, is arranged for the reception of the water which falls upon its
receiving surface only, and for the prevention of loss by evaporation. The
rain is first collected in a funnel, _B_, (fig. 84,) the receiving surface
of which is turned in a lathe. The conical surface of the funnel slopes to
the pipe, _E_, at an angle of 60 deg. from the horizontal receiving surface.
The tube, _E_, is of small aperture, and is bent up, in order to retain
the last few drops of rain, so that the only opening for the escape of
vapour may be closed as long as possible. The funnel, _B_, fits upon the
cylinder, _A_, tightly in the groove, _D_. A copper can is placed inside
the cylinder, _A_, to receive the rain from the funnel. Once or twice a
day, or after a shower, this can should be taken out, and the water
measured in the glass measure, _C_, which is graduated to hundredths of an
inch, according to the calculated quantity of water, determined by the
area of the receiving space. In use, this gauge should be partly sunk in
the ground, so that the top may be about five inches above it. Thus
situated, there will be little or no evaporation from it during any month
of the year; and the readings need not be taken daily, although desirable.


=112. Rain-Gauge with Float.=--In this construction the graduated glass
measure is dispensed with. The cylinder of the gauge is made less in
diameter than the funnel, and a hollow, very flattened spheroid of copper
forming a float, and carrying a vertical graduated boxwood scale which
moves through the orifice of the funnel, is placed in it. As the rain
accumulates the float rises, and the amount of rain in the gauge is read
upon the scale from the top of the gauge, a bar, having a hole at the
centre for the passage of the scale, being fixed diametrically across the
receiving space of the funnel. The gauge is provided at the bottom with a
brass cock, by which the water may be allowed to flow out of it whenever
necessary.

This form of gauge is not very suitable for the measurement of small
quantities; but is admirably adapted for localities where the rainfall is
excessive.


[Illustration: Fig. 85.]

=113. Rain-Gauge with Side-Tube.=--This instrument, as represented in fig.
85, is a cylindrical vessel, mounted on a base shaped as a frustum of a
cone. This base may be filled with sand or gravel to make the instrument
stable, so that when placed upon a lawn or in a garden it may have an
ornamental appearance. The funnel for collecting the rain is larger in
diameter than the cylinder. Parallel to the cylinder, and communicating
with the lowest part of the interior and extending to its top, is a
graduated glass tube, open at both ends. The rain collected will rise as
high in this tube as in the cylinder, and its amount can therefore be read
off without any trouble. The gauge is emptied by the brass tap at the
bottom of the cylinder.


=114. Admiral FitzRoy's Rain-Gauge.=--A form of rain-gauge, very well
adapted for expeditious observation at any time, has been designed by
Admiral FitzRoy, and extensively employed by his observers. It is
cylindrical in shape, with the funnel let into the top; and the rainfall
is collected in an inner and much smaller cylinder, so that a small fall
is represented by a considerable depth of water in the gauge. The amount
of rain which has fallen is ascertained by a dipping tube, similar in
principle to the dipping syphon used by gaugers for taking out specimens
of wines or spirits from casks by simply removing the bung. A short,
vertical, tubular opening provided with a cap, which is attached to the
instrument by a chain that it may not be lost, is formed in the funnel.
The measuring tube, which has a small hole at each end, should be placed
upright in the gauge; then the thumb should be pressed over the upper
aperture, while the tube is lifted gently out, holding in the lower part a
quantity of water representing the depth of the rain in the gauge, the
upper edge of which is at the mark to be read off. The glass tube is
graduated to inches and tenths; hundredths of an inch can be readily
estimated by the eye. The marks are fixed by actual trial with a standard
gauge, and are artificial, not true, inches.


=115. Self-Registering Rain-Gauge.=--The rain-gauge can be combined with
clock-work and other mechanism so as to be self-recording of the amount of
rain, the time, and duration of its fall. For the details of construction
the reader is referred to the next chapter, where he will find the
instrument described in connection with Osler's anemometer, as the
"pluviometer." To observe and duly record the times of commencement and
termination of rain is very desirable. Scarcely any observer can attempt
to do this even approximately from personal observation. Hence the want of
a cheap and simple self-recording rain-gauge is much felt, the present
construction being too expensive for all but a few individuals.

In 1862, Mr. R. Strachan estimated the duration and amount of rain in
London (Gray's Inn Road) as follows:--

  +-------------------------------------------------------------------+
  |  MONTHS.  |INCHES.|DAYS.|HOURS.||  MONTHS.   |INCHES.|DAYS.|HOURS.|
  |-----------+-------+-----+------++------------+-------+-----+------|
  |January.   | 1.86  | 19  |  88  ||July.       | 2.27  | 17  |  68  |
  |February.  | 0.37  |  9  |  25  ||August.     | 2.45  | 12  |  72  |
  |March.     | 3.40  | 22  | 130  ||September.  | 1.70  | 12  |  55  |
  |April.     | 2.34  | 14  |  80  ||October.    | 3.23  | 21  |  94  |
  |May.       | 3.04  | 16  |  90  ||November.   | 1.12  | 10  |  53  |
  |June.      | 2.45  | 20  |  83  ||December.   | 1.44  | 17  |  66  |
  +-------------------------------------------------------------------+

"During the year 1862, the rainfall amounted to 25.67 inches. Rain fell on
179 days, that is, on nearly every other day. The hours of rain were
estimated at 904; therefore, if the rain had fallen continuously, it would
have lasted nearly 38 days and nights."[10] The value of similar estimates
of the rainfall by numerous observers would be very great to meteorology.


=116. The principle of measurement= in all these gauges is the relation
existing between the areas of the collecting and receiving surfaces; that
is, between the area of the funnel into which the rain falls, and the area
of the cylinder which receives it. In Howard's and Glaisher's gauges, this
cylinder is virtually the measuring glass itself; in the others, above
described, the measuring scales show the same depth of water as in the
cylinder of the gauge.

The cylinder being of less diameter than the funnel, and receiving all the
rain collected by the funnel, it follows that its contents will have an
increased depth. Now equal cylindrical volumes, having different
diameters, are to each other in length inversely as the squares of the
diameters. Hence, if the funnel be 9 inches and the cylinder 3 inches in
diameter, a fall of 1 inch of rain will be represented in the gauge by 9
inches; for 3 squared : 9 squared :: 1 : _x_ = 9. In this case, therefore, a length of
nine inches of the measuring glass, tube, or scale, would represent an
inch of rainfall, and be divided into tenths and hundredths of the
artificial inch.


=117. Position for Rain-Gauge, &c.=--Rain gauges should be placed on the
ground, in any position exposed to a free fall of rain, snow, or hail,
where neither walls, buildings, nor trees shelter or cause eddies of wind.
They should be supported by a frame, or other means, to prevent them being
blown down by the wind, but so that they can be readily emptied.

During snow or frost, the gauge must be watched, and its contents melted
by placing it in a warm room, either when the amount is to be measured, or
the funnel is filled up with snow. A tin vessel of equal area to the
funnel may at such times be useful as a substitute.

Rain gauges are constructed of metal, usually copper, which, besides being
readily workable, is little affected by atmospheric influences. If made of
iron or zinc, they should be well japanned; if of copper, this is not so
essential. The capacity of a gauge should be sufficient to contain at
least the probable maximum fall of rain in a day at the locality. Those
required for rainy districts must be of large size.


=118. Causes of Rain.=--When the invisible vapour which is diffused in the
atmosphere becomes sufficiently cooled, it appears visible as mist or
cloud, and a further reduction of temperature causes its precipitation as
rain, hail, or snow. The cooling of the higher regions of the atmosphere
is doubtless the chief cause of this condensation; but the property which
aqueous vapour possesses of radiating heat may also contribute to the
result. Moreover, the law which regulates the amount of vapour which air
at any particular temperature can sustain in a transparent state,
determines that when two bodies of air at different temperatures,
saturated with vapour, intermix, some moisture must be rendered visible;
and hence, it is not only possible, but highly probable, that rain may
result from the conflict of different winds. Let us imagine two cubic
yards of air, both saturated with moisture, but having the respective
temperatures of 50 and 70 degrees, to come into contact. There will be a
tendency to equalize the temperature to a mean, which is 60 deg.; and during
this process, some of the vapour will be condensed.

  For in the air at 50 deg. there is                     110.7 grains of vapour[11]
  and       "       70      "                        216.0       "
                                                    ------
  Total amount of vapour                             326.7       "
  But two cubic yards of air at 60 deg. can only sustain 313.2       "
                                                    ------
  Hence there will be deposited                       13.5       " of rain.
                                                    ======

It may be conceded, therefore, that when a warm and moist current of air
encounters a body of cold air which may not be extremely dry, the mixture
is unable to retain the whole of the vapour in an invisible state; so that
the excess becomes visible as mist or fog, and, when the temperature has
become sufficiently lowered, rain. The British Isles are more or less
enveloped in fog, or mist, at the commencement of easterly winds, which,
with a sudden change of wind, is exhibited even in summer; while the
south-westerly winds, warm, and arriving from the ocean, deposit large
quantities of rain by the cooling effect of the land, colder by reason of
its latitude. When rain occurs with a northerly wind, it is probably due
to the deposition from an upper south-westerly current, often apparently
proved by the movements of the upper clouds.


=119. Laws of Rain-fall.=--Tropical countries have a dry and a wet season
during the year: _dry_, when the sun is at the opposite side of the
equator; _wet_, when the sun is overhead. With reference to the British
Isles, the statistics collected by Mr. G. J. Symons indicate that: 1st.
The stations of least rain are inland, or on the east or south-east
coasts; the stations of greatest rain are on the western coasts. 2nd. The
rain-fall is very large in the vicinity of mountain chains or groups,
unless the station happens to be some miles to the north-eastward.

It may be well to illustrate these remarks by quoting[12] the average fall
at a few places, grouping them as--

      Westerly.
                           Inches.
  Bodmin                    43
  Bolton (Lancashire)       44
  Coniston (Windermere)     71
  Seathwaite               127
  Torosay (I. of Mull)      75
  Killaloe (Limerick)       38

     Central.
                           Inches.
  Enfield                   23
  Epping                    23
  Derby                     24
  York                      22
  Stirling                  39
  Perth                     29

     Easterly.
                           Inches.
  Witham (Essex)            21
  Patrington (Hull)         21
  Sunderland                17
  Inveresk (Edinburgh)      25
  Pittenweem (Fife)         24
  Dublin                    22

Mr. Green, the celebrated aeronaut, has asserted from his experience,
"that whenever a fall of rain happens, and the sky is entirely overcast,
there will invariably be found to exist another stratum of cloud at a
certain elevation above the former;" and the recent scientific balloon
ascents by Mr. Glaisher have tended to confirm this theory. Mr. Glaisher
says, "It would seem to be an established fact, that whenever rain is
falling from an overcast sky, there is a second stratum above." "It would
also seem that when the sky is overcast without rain, that there is no
stratum of cloud above, but that the sun is shining on the upper surface.
In every instance in which I have been up under these circumstances, I
have found such to be the case, agreeing in this respect also with Mr.
Green's observations."

The amount of rain collected in a gauge placed near the surface of the
earth is larger than in any gauge placed above it; and the higher the
gauge is placed, the less water is collected. Mr. Glaisher contends that
his balloon experiments corroborate this law.


=120. Utility of Statistics of Rain-fall.=--The utility of knowing the
rain-fall of any locality is sufficiently obvious, and little need be said
upon the subject. The rain-gauge should be in the hands of every gardener
and farmer. In the management of out-door plants and crops, as well as in
the construction of cisterns and tanks for the supply of water, a rain
gauge is a valuable assistant. By its use, the gardener will be guided in
judging how far the supply of moisture to the earth is needed; and he will
also see how beneficial is even a hasty shower to growing plants, when he
considers that a fall of rain measuring the tenth of an inch in depth,
corresponds to the deposit of about forty hogsheads per acre. The study of
the rain-fall of a country is of considerable interest to agriculturists.
The health and increase of domestic animals, the development of the
productions of the land, as well as the daily labours of the farmer, are
dependent upon the excess or deficiency of rain. "It must be a subject of
great satisfaction and confidence to the husbandman to know at the
beginning of a summer, by the certain evidence of meteorological results
on record, that the season, in the ordinary course of things, may be
expected to be a dry and warm one; or to find, in a certain period of it,
that the average quantity of rain to be expected for the month has fallen.
On the other hand, when there is reason, from the same source of
information, to expect much rain, the man who has courage to begin his
operations under an unfavourable sky, but with good ground to conclude,
from the state of his instruments and his collateral knowledge, that a
fair interval is approaching, may often be profiting by his observations;
while his cautious neighbour who waited 'for the weather to settle' may
find that he has let the opportunity go by. This superiority, however, is
attainable by a very moderate share of application to the subject; and by
the keeping of a plain diary of the barometer and rain-gauge, with the
hygrometer and vane, under his daily notice."[13] The statistics of
rain-fall are not only valuable and interesting in a meteorological point
of view, and for agricultural purposes, but are also highly important in
connection with sanitary arrangements for towns, and engineering
operations. This is especially evident to the hydraulic engineer. As rain
is an important source of water-supply to rivers, canals, and reservoirs,
it is evident that a knowledge of the probable fall for any season or
month, at a given place, as furnished by averages of the observations of
former years, will be the data upon which the engineer will base his plans
for providing for floods or droughts; while the measurement of the actual
quantity which has just fallen, as gathered from the indications of a
series of gauges, will suggest to him the precautions to adopt either to
economise or conduct away the in-pouring waters.

"When a canal is conducted across an undulating country, its course is
necessarily governed by the accidents of the ground, and it alternately
rises and falls. In this case, rising by a succession of levels, it
necessarily arrives at a certain highest level, which is called by
engineers the _summit level_. From this it again descends by a
corresponding series of levels. Now, it is evident that, supposing the
locks to be all equal in magnitude, the ascent of a vessel will require
the descent of as much water from the summit to the lowest level as would
fill a single lock; for this quantity of water must be discharged from
each lock of the series when the vessel passes through it.

"The same may be said of the process by which the vessel descends along
the series of locks on the other side of the summit. It appears,
therefore, that a supply of water must always be maintained on the summit
level sufficient to fill a single lock twice for each vessel which crosses
the summit.

"It happens, fortunately, that by the laws of natural evaporation, rain is
precipitated in greater quantities on elevated summits than on the
intermediate valleys, so that the moving power, in this case, accommodates
itself to the exigencies of intercommunication."--_Dr. Lardner's "Handbook
of Natural Philosophy."_


=121. New Form of Rain-Gauge.=--Since the foregoing pages were in type, a
modification of Howard's rain-gauge has been arranged by Mr. Symons, which
is compact in design, convenient in use, and low in price. It combines the
advantages of most gauges; having solidity, and facility of measurement.
The bottle is placed in a tin case, to the bottom of which are attached
stout spikes, which, when forced into the earth, prevent its being upset
either by wind or accident. The bottle being transparent, and slits made
in the case, the fall of rain is seen at a glance, or with a race-glass,
from a window. The funnel being attached to the cover of the case is
thereby kept strictly horizontal, and the depth of rain can be accurately
measured by lifting the bottle from its case and emptying it into a
graduated glass jar.

The funnel of this gauge is a very deep cone, to prevent the rain drops
outsplashing. When properly placed, the receiving surface will be twelve
inches above the ground, which experience has shown to be the most
advantageous height.




CHAPTER XIII.

APPARATUS EMPLOYED FOR REGISTERING THE DIRECTION, PRESSURE, AND VELOCITY
OF THE WIND.


=122. The Vane.=--The instrument by which the wind's direction is most
generally noted, is the vane, or weather-cock, and all that need be said
of it here is that the points north, east, south and west, usually
attached to it, should indicate the _true_ and not the _magnetic_
directions; and that care should be taken to prevent its setting fast.
Very complicated instruments are required for ascertaining the pressure
and velocity of the wind, and these are called _Anemometers_. The simplest
is _Lind's_.


[Illustration: Fig. 86.]

=123. Lind's Anemometer, or Wind-Gauge= (fig. 86), invented so late as
1775, for showing the pressure of the wind, consists of a glass syphon,
the limbs parallel to each other, and each limb the same diameter. One end
of the syphon is bent at right angles to the limb, so as to present a
horizontal opening to the wind. A graduated scale, divided to inches and
tenths, is attached to the syphon tube, reading either way from a zero
point in the centre of the scale. The whole instrument is mounted on a
spindle, surmounted by a vane, and is moved freely in any direction by the
wind, always presenting the open end towards the quarter from which the
wind blows. To use the instrument, it is simply filled up to the zero
point with water, and then exposed to the wind; the difference in the
level of the water gives the force of the wind in inches and tenths, by
adding together the amount of depression in one limb, and elevation in the
other, the _sum of the two_ being the height of a column of water which
the wind is capable of sustaining at that time.

TABLE,

Showing the Force of Wind on a square foot, for different heights of the
column of Water in Lind's Wind-Gauge.

  +-----------------------------------+
  |Inches.|Force in|Common designation|
  |       |  lbs.  |   of such Wind.  |
  |-------+--------+------------------|
  |  6    |  31.75 | A Hurricane.     |
  |  5    |  26.04 | A violent Storm. |
  |  4    |  20.83 | A great Storm.   |
  |  3    |  15.62 | A Storm.         |
  |  2    |  10.42 | A strong Wind.   |
  |  1    |   5.21 | A high Wind.     |
  |   .5  |   2.60 | A brisk Wind.    |
  |   .1  |    .52 | A fresh Breeze.  |
  |   .05 |    .26 | A gentle Breeze. |
  | 0.    |   0.   | A Calm.          |
  +-----------------------------------+


=124. Modification of Lind's Gauge.=--_Sir W. Snow Harris_ has effected a
modification of Lind's anemometer, with a view of obtaining a hand
instrument for use at sea more especially. At present the force of the
wind is estimated at sea by an arbitrary scale, suggested by Sir F.
Beaufort, the late hydrographer; 0 being calm, 12 the strongest hurricane,
and the intermediate numerals giving the varying strength of the wind.
There has been a long-felt want of instrumental means for obtaining this
data at sea, if merely for the sake of checking occasionally personal
estimations, which may vary considerably among different observers.
Harris's wind gauge is intended to be held by hand, while facing the wind,
and keeping it in proper position by attending to a spirit-level attached.
When in position, and held firmly, the tube has to be opened to the wind
by pressure of the thumb acting upon jointed levers, controlled by
springs. The pressure of the wind moves the enclosed liquid; and by
withdrawing the thumb, the tube is closed so as to keep the liquid in its
position; the reading is then taken from its scale, either in pounds on
the square foot, miles per hour, or the ordinary designations of wind, as
light, fresh, strong, &c.


=125. Robinson's Anemometer.=--_Dr. Robinson_, of Armagh, is the inventor
of a very successful anemometer, which determines the horizontal velocity
of the wind. It was first used in 1850, in the meteorological and tidal
observations made on the coast of Ireland under the direction of the Rev.
Dr. Lloyd. No meteorological observatory should be without this valuable
instrument, which is essential in determining the average velocity of the
wind of a locality as distinguished from the most frequent wind of the
same place. It is represented in fig. 87. Four hollow hemispherical cups,
_A A_, are extended upon conjugate diameters, or arms, with their
diametrical planes placed vertically, and facing the same way upon a
vertical axis, _B_, which has at its lower extremity an endless screw,
_D_. The axis is supported at _C_ so as to turn with as little friction as
possible. The endless screw is placed in gear with a train of wheels and
pinions. Each wheel carries an index over a stationary dial in front; or
the index is fixed, and the graduations are placed upon the wheels
themselves.

[Illustration: Fig. 87.]

Dr. Robinson has proved, both by theory and experiment, that the centre of
any one of the cups so mounted and set in motion by the wind, revolves
with one-third of the wind's velocity. If, therefore, the diametrical
distance between the centres of the cups be one foot, the circle described
by the centres in one revolution is 3.1416 feet, and the velocity of the
wind will be three times this, or 9.42 feet, which must be referred to
time for the absolute rate. The instrument is sometimes made with the
centres of the cups 1.12 feet apart, so that the circle described is
1/1500 of a mile in circumference. Hence, to produce one revolution of the
cups, the wind must travel three times as fast, or 1/500 of a mile.
Therefore, 500 revolutions will be produced by one mile of wind; so that
the dials may be graduated to register the velocity in miles and tenths of
miles. The simplest arrangement is with five dials, recording respectively
10, 100, 1,000, 10,000 and 100,000 revolutions.

_Directions for using Robinson's Anemometer._--The dials read off in the
same manner as the register of a gas meter, commencing with the dial
farthest from the endless screw.

"The figures on the first dial indicate so many hundreds of thousands of
revolutions; those on the second dial so many tens of thousands; those on
the third, thousands; those on the fourth, hundreds; and those on the
fifth so many tens.

"The instrument should be read every morning at 9 o'clock; and, usually,
it will only be necessary to read the first three dials. The figures can
be entered as they are read off. Should the index point _between_ two
figures, the less of the two is to be taken.

"For example, if the first dial points to 7, or between 7 and 8; while the
second dial indicates 4; and the third, 5; the entry to be made is 745
(indicative of 745 _thousand_ revolutions).

"Every time the index of the first dial is found to have passed zero (0),
a cross or star is to be prefixed to the next (a lower) reading.

"To ascertain how many _thousands_ of revolutions have been made during
the month, it will simply be necessary to subtract the first reading from
the last, and prefix to the three figures thus obtained a figure
corresponding to the number of stars in the column. For every _thousand_
revolutions there are two miles of wind: we have therefore only to
multiply by 2 to find how many miles of wind have passed during the month.

"Two entries must be made for the last day of each month (the one being
written under the other), so as to bring the readings down to 9 A.M. on
the 1st of the following month. The same entry which ends one month, will
therefore begin the next. This repetition of one entry is necessary, in
order to prevent losing a day's wind.

  "The accompanying example of the           687
  readings of an Anemometer for 13 days      773
  will illustrate the method of making       822
  the entries, &c.                           855
                                             900
  "In this instance, the first reading       953
  (687) is less than the last (793).         990
  When the first reading is greater than    *066
  the last, it will be necessary to borrow   197
  1,000 in making the subtractions,          323
  and then deduct one from the number        414
  of stars. Thus, if the first reading       597
  of the series on the margin had            712
  been 887, the result would have been       793
  906 instead of 1106.                      ----
                                            1106 thousands of revolutions.
                                               2
                                          +-----
                                       13 | 2212 miles of wind in period.
                                          +-----
                                             170 miles of wind per day, on
                                                 an average.

"The foregoing directions are all which require to be regularly attended
to. But it may be interesting at times to find the velocity of the wind
during a period of a few minutes. This may be ascertained by observing the
difference of two readings of all the dials, with an interval of some
minutes between them, when a very brief calculation will suffice; but
perhaps the simplest method is the following:--

"Take two readings, with an interval of 12 minutes between them. The
difference of these readings, divided by 10, is the velocity of the wind
in miles per hour. Thus--if the reading of the five dials (from left to
right) at noon is 15206, and at 12 minutes past 12 is 15348, the velocity
of the wind is 14.2 miles per hour."--_Admiral FitzRoy, F.R.S._

A lever and clutch are sometimes fitted to this anemometer, as in fig. 88,
for throwing the train out of gear when not required to register. It may
also be connected with clock-work so as to be self-recording, by causing
the mechanism to impress a mark upon prepared paper moved by the
apparatus, at certain intervals of time.

[Illustration: Fig. 88.]

This anemometer should be fixed in an exposed situation, as high above
ground as may be convenient for reading. It may be made very portable, by
the arms which carry the cups being fitted to unscrew or to fold down.
When fitted in gimbals, it can be used at sea with much advantage.

The pressure of the wind has been experimentally proved to vary as the
square of the velocity; the relation being _V squared_ = 200 x _P_. From this
formula, therefore, the pressure can be calculated corresponding to the
observed velocity.


=126. Whewell's Anemometer.=--This apparatus, the invention of the
celebrated Dr. W. Whewell, registers the horizontal motion of the air with
the direction. Its mechanism may be described in general terms, as
follows:--

A horizontal brass plate is attached to a vertical spindle, which passes
through the axis of a fixed cylinder, being supported by a bearing at the
lower end, and working in a collar at the upper. A vane is attached, by
which the plate is moved about according to the direction of the wind. A
fly, having eight fans, each fixed at an angle of 45 deg. with the axle, is
placed upon the plate so that the axle is in the line of direction of the
vane. An endless screw on the axle turns a vertical wheel having one
hundred teeth, the axle to which has also an endless screw working into a
horizontal wheel, having a like number of teeth, and which communicates
motion to a vertical screw fifteen inches long. On this screw is placed a
moveable nut, which carries a pencil. Round the cylinder is wrapped daily
a paper divided for the points of the compass. The wind acting upon the
vane will cause the plate to turn; and the screw which carries the pencil
will travel with it, so that the pencil will mark upon the paper the
direction of the wind. The fly will also be set in motion, and thereby the
nut upon the screw will descend, so that the attached pencil will trace a
vertical line upon the paper. When the fans on the axle are 2.3 inches
from axis to end, and 1.9 inches wide, and the thread of the screw such
that forty-five revolutions will cause the nut to descend two inches,
75.85 miles of wind will cause the pencil to descend through a vertical
space of two inches; but the actual trace upon the paper will be longer in
proportion to the magnitude of change of azimuth, or direction, of the
wind.


=127. Osler's Anemometer, and Pluviometer.=--Mr. Follet Osler is the
inventor of a self-recording apparatus which registers the direction and
pressure of the wind, and the amount and duration of rain, upon the same
sheet of paper. His apparatus has met with very much approbation, and has
been erected in many observatories. The mechanism may be modified in
various ways, and the following is a description of the simplest and most
recent arrangement.

[Illustration: Fig. 89.]

The instrument, of which fig. 89 is a diagram rather than a picture,
consists, first, of a vane, _V_, of a wedge-shape form, which is found to
answer better than a flat vane; for the latter is always in a neutral
line, and therefore is not sufficiently sensitive. A wind-mill governor
has been substituted for the vane to get the direction of the wind, with
advantage. At the lower end of the tube, _T T_, is a small pinion, working
in a rack, _r_, which moves backwards and forwards as the wind presses the
vane. To this rack a pencil, _x_, is attached, which marks the direction
of the wind on a properly ruled paper, placed horizontally beneath, and so
adjusted as to progress at the rate of half an inch per hour, by means of
a simple contrivance connecting it with a good clock. The paper is shown
in the illustration upon the table of the instrument.

The pressure plate, _F_, for ascertaining the force of the wind, is one
foot square, placed immediately beneath, and at right angles with the
vane; it is supported by light bars, running horizontally on friction
rollers, and communicating with flattened springs, 1, 2, 3, so that the
plate, when affected by the pressure of the wind, acts upon them, and they
transfer such action to a copper chain passing down the interior of the
direction tube, and over a pulley at the bottom. A light copper wire
connects this chain with the spring lever, _y y_, carrying a pencil which
records the pressure upon the paper below. Mr. Osler much prefers a spring
to any other means for ascertaining the force of the wind, because it is
of the highest importance to have as little matter in motion as possible,
otherwise the momentum acquired will cause the pressure plate to give very
erroneous indications. The pressure plate is as light as is consistent
with strength. It is kept before the wind by the vane, and is urged out by
three or more springs, so that with light winds one only is compressed,
and two, or more, according to the strength of the wind.

The _pluviometer_ is placed on the right in the figure, _P P_ being the
plane of the roof of the building. The rain funnel, _R_, exposes an area
of about 200 square inches. The water collected in it is conveyed by a
tube through the roof of the building into a glass vessel, _G_, so
adjusted and graduated as to indicate a quarter of an inch of rain for
every 200 square inches of surface, _i. e._ 50 cubic inches. _G_ is
supported by spiral springs, _b b_, which are compressed by the
accumulating rain. A glass tube, open at both ends, is cemented into the
bottom of _G_, and over it is placed a larger one closed at the top like a
bell glass. The smaller tube thus forms the long leg of a syphon, and the
larger tube acts as the short leg. The water, having risen to the level of
the top of the inner tube, drops over into a little copper tilt, _t_, in
the globe, _S_, beneath the reservoir. This tilt is divided into two equal
partitions by a slip of copper, and placed upon an axis not exactly
balanced, but so that one end or the other preponderates. The water then
drops into the end of the tilt which happens to be uppermost, and when
quite full it falls over, throwing the water into the globe, _S_, from
which it flows away by the waste pipe. In this way an imperfect vacuum is
produced in the globe, quite sufficient to produce a draught in the small
tube of the syphon, or the long leg; and the whole contents of the
reservoir, _G_, immediately run off, and the spiral springs, _b b_,
elevate the reservoir to its original position. To produce this action, a
quarter of an inch of rain must have fallen. The registration is easily
understood. A spring lever, _z_, carrying a pencil, is attached by a
cord, _c_, to _S_. This spring always keeps the cord tight, so that as the
apparatus descends during the fall of rain, the spring advances the pencil
more and more from the zero of the scale upon the paper beneath, until a
quarter of an inch has fallen, when the pencil is drawn back to zero by
the ascent of the reservoir.

The clock movement carries the registering paper forward by one of the
wheels working into a rack attached to the frame.

The adjustment of the instrument should be carefully made at its first
erection. The scale for pressure should be established experimentally, by
applying weights of 2, 4, 6, &c., lbs., to move the pressure plate.

The registration trace for twenty-four hours is readily understood. The
direction is recorded on the centre part; the pressure on one side, and
the rain on the other. Lines parallel to the length of the paper show no
rain, steady wind, and constant pressure. On the rain trace, a line
parallel to the width of the paper shows that the pencil had been drawn
back to zero, a quarter of an inch of rain having fallen. The hour lines
are in the direction of the width of the paper.

At the International Exhibition 1862, Messrs. Negretti and Zambra
exhibited an improved Osler's anemometer, having combined with it
Robinson's cups, so that the pressure and velocity appear on the same
sheet, on which a line an inch in length is recorded at every ten miles;
thus the complete instrument shows continuously the direction, pressure,
and velocity of the wind.


=128. Beckley's Anemometer.=--Mr. R. Beckley, of the Kew Observatory, has
devised a self-registering anemometer, which consists of three principal
parts: Robinson's cups for the determination of velocity; a double fan, or
wind-mill governor, for obtaining the direction; and a clock to move a
cylinder, around which registration paper is wrapped. The paper records
the time, velocity, and direction of the wind for twenty-four hours, when
it must be replaced. It has a cast-iron tubular support, or pedestal to
carry the external parts--the cups and the fans,--which must be erected
upon the roof of the building upon which it is desired to mount the
instrument.

The fans keep their axis at right angles to the wind; and with any change
of direction they move, carrying with them an outer brass tube, which
rests upon friction balls on the top of the pedestal, and is attached to a
tubular shaft passing through the interior of the pedestal, and
terminating with a mitre wheel. The mitre wheel, working with other cogged
wheels, communicates the motion of the direction shaft to a cylinder
carrying a pencil, to record the direction.

The shaft carrying the cups is supported upon friction balls, placed in a
groove formed on the top of the direction shaft, and passing through the
interior of that shaft, comes out below the mitre wheel, where it is
terminated in an endless screw, or worm.

Upon the wind moving the cups, motion is given to the innermost shaft,
thence to the worm-wheel, whence motion is given to a pencil which
registers the velocity.

De la Rue's metallic paper is used in registration, it having the property
of receiving a trace from a brass pencil. The pencils can, therefore, be
made in the most convenient form. Mr. Beckley forms each pencil of a strip
of brass wrapped round a cylinder, making a very thin threaded screw, so
that the contact of the pencil cylinder and the clock cylinder is a mere
point of the metallic thread. The pencil cylinders are placed side by side
upon the cylinder turned by the clock, and require no spring or other
appliance to keep them to their work, but always make contact with the
registration paper by their own gravity. They therefore require no
attention, and being as long as the trace which they make, they will last
a long time.

The velocity pencil has only one turn on the cylinder, and its pitch is
equal to a scale of fifty miles upon the paper. The direction pencil has
likewise one turn on its cylinder, its pitch being equal to a scale of the
cardinal points of the compass upon the paper.

The clock gives a uniform motion of half an inch per hour to the cylinder
upon which the paper is fastened.

The registering mechanism of the instrument is very compact, requiring
only a space of about 18 inches by 8 inches.

In the Report of the British Association for 1858, Mr. Beckley has given a
detailed description of his anemometer, with drawings of all the parts.


=129. Self-Registering Lind's Anemometer.=--A Lind's wind-gauge, designed
to register the maximum pressure, was exhibited at the International
Exhibition 1862, by Mr. E. G. Wood. The bend of the syphon is contracted
to obtain steadiness. On the leeward limb a hole is drilled corresponding
in size with the contracted portion of the tube. The edge of the hole
corresponds with the zero of the scale. On the pressure of the wind
increasing, as much of the water as would have risen above the aperture
flows away, and therefore the quantity left indicates the greatest
pressure of the wind since the last setting of the instrument, which is
done by filling it with water up to the zero point.


=130. Anemometric Observations.=--To illustrate the value of anemometric
observations, we quote from a paper by Mr. Hartnup, on the results
obtained from Osler's Anemometer, at the Liverpool Observatory. The six
years' observations, ending 1857, gave for the yearly average of the
winds: North-easterly, on 60 days, at 7.8 miles per hour; North-westerly,
on 112 days, at 15.4 miles per hour; South-easterly, on 115 days, at 11.0
miles per hour; South-westerly, on 77 days, at 13.8 miles per hour; and
one day calm. From the same observations, the average variation in the
strength of the wind during the 24 hours is:--11 miles per hour, the
minimum force, occurring at 1-1/2 a.m.; until 6 a.m. it remains much the
same, being then 11.3 miles per hour; at 10 a.m. it is 13.4 miles per
hour; at 1-1/2 p.m. the wind is at its maximum strength, being 14.8 miles
per hour; at 5 p.m. it is again 13.4 miles per hour, and at 9 p.m. 11.3
miles per hour. Hence it appears that the wind falls to its minimum force
much more gradually than it rises to its maximum; that the decrease and
increase are equal and contrary, so that the curve is symmetrical; and
that generally the force of wind is less at night than during the day.

"There is evidence," says Admiral FitzRoy, "in Mr. Hartnup's very valuable
anemometrical results, which seems to prove that to his observatory, in a
valley, with buildings and hills to the north-eastward, the real polar
current does not blow from N.E., but nearer S.E. By his reliable digest of
winds experienced there, it appears that those most prevalent were from
W.N.W. and S.S.E. But in England, generally, the _prevailing_ winds are
_believed_ to be westerly, inclining to south-westerly, and
north-easterly; while of all winds, the south-easterly is about the
rarest.

"At Lord Wrottesley's observatory, in Staffordshire, about 530 feet above
the sea, there appears to be considerably less strength of wind at any
given time, when a gale is blowing _generally_, than occurs simultaneously
at places along the sea-coast: whence the inference is, that undulations
of the land's surface and hills, diminish the strength of wind materially
by frictional resistance.

"All the synoptic charts hitherto advanced at the Board of Trade exhibit a
marked diminution of force inland compared with that on the sea-coast.
Indeed, the coast itself offers similar evidence, in its stunted, sloping
trees, and comparative barrenness."[14]




CHAPTER XIV.

INSTRUMENTS FOR INVESTIGATING ATMOSPHERIC ELECTRICITY.


=131. Atmospheric Electroscope.=--The simplest instrument for ascertaining
at any time the electric condition of the atmosphere is an electroscope
composed of two equal pieces of gold leaf, suspended from a brass support,
and insulated, as well as protected from the movement of the air, by a
glass covering. Fig. 90 represents such an instrument. The cap of the
brass support is fitted for the reception, in the vertical direction, of a
metallic rod, not less than two or three feet in length. The top of the
rod carries a clip. The instrument acts according to the law, that bodies
similarly electrified repel each other; but when dissimilarly electrified,
they attract each other. To make an observation, the instrument is placed
in the open air, and a lighted piece of cigar fusee, or touch-paper, is
fixed in the clip. The electricity of the air is collected by the
substance undergoing combustion, and conducted by the rod to the gold
leaf; and the pieces, being similarly electrified, separate more or less
according to the amount of electricity present. The kind is determined by
the effect of either an excited stick of sealing-wax or rod of glass upon
the electrified gold leaf. A rod of glass, when rubbed briskly with a silk
handkerchief or piece of woollen cloth, becomes positively electrified, or
excited, as it is termed. A stick of sealing-wax, similarly treated,
acquires the negative state. If, therefore, an excited glass rod be
presented to the cap of the instrument, and it cause the pieces of gold
leaf to diverge still further, the electric state of the air must be
analogous to that of the glass, that is, _positive_; if they approach, it
is _negative_. On the contrary, if a stick of sealing-wax be used, the
pieces will be repelled more apart if they have acquired negative
electricity from the air; and they will converge if they have a positive
charge.

[Illustration: Fig. 90.]

By means of this very simple instrument, meteorological observers can
readily ascertain the electric condition of the lower air at any time.

NOTE.--A book containing strips of gold leaf is sent with the Electrometer
to replace the gold leaves when torn or broken in use.

To mount fresh gold leaves, unscrew the brass plate to which is attached
the rod supporting the leaves; then moisten with the breath the flat piece
of brass, and press it gently down on one strip of gold, whilst the book
is only partly opened; the second leaf is attached in the same manner.


=132. Volta's Electrometer= is similar to the instrument just described,
except that instead of gold leaf two light pieces of straw, or two pith
balls, are freely suspended from the conductor; the amount of the electric
charge being estimated from the degrees of divergence, shown by a
graduated arc.


=133. Peltier's Electrometer= is a much superior instrument in point of
sensibility. A tall glass tube an inch or more in diameter, is connected
to a glass receiver, mounted on a base fitted with levelling screws. At
the top of the tube is formed a globe from four to five inches in
diameter, which is thickly gilt on the exterior, so as to form a good
conducting surface. A wire passes from the ball down the tube into the
receiver, where it is bent up, and ends in a steel point over the centre
of the base. A bent wire, carrying a small magnetic needle, is balanced on
the steel point, so that the magnet, with the fine wire, arranges itself
horizontally in the direction of the magnetic meridian. If any cloud or
portion of air in the neighbourhood be in an electrical state, it will act
by induction upon the gilt ball, and the needle will be deflected from its
north and south direction.

A graduated circle indicates the number of degrees of the deflection,
which will be greater or less according to the tension of the electricity.
To ascertain whether the electricity is positive or negative, a stick of
shellac or glass must be employed, as already described.


=134. Bohnenberger's Electroscope= may be fitted with a metallic
conductor, and used with great advantage for observing atmospheric
electricity. "The principal parts of the instrument, as improved by
Becquerel, are the following:--_A B_, fig. 91, is a small dry galvanic
pile of from 500 to 800 pairs, about a quarter of an inch in diameter;
when the plates are pressed together, such a pile will be from 2 to 2-1/2
inches in length. The wires, which are bent so as to stand above the pile,
terminate in two plates, _P_ and _M_, which are the poles of the pile.
These plates, which are 2 inches by 1/2 an inch, are parallel and opposite
to each other. It is convenient for their opposite sides to be slightly
convex, for them to be gilded or coated with platinum, and for them to run
on the polar wires, by the latter being made to pass through a small hole
in them. One of these plates will always be in a state of positive, and
the other of negative, electricity; between them suspend the very fine
gold leaf, _D G_, which is attached to the conductor, _C D_, of copper
wire. If the leaf hang exactly between the two plates, it is equally
attracted by each, and will therefore be in a state of repose. The
apparatus should be protected by a bell-glass, fitting exactly, and having
an opening at the top through which the copper wire, _C D_, passes; the
wire, however, is insulated by its being contained in a glass tube, which
is made to adhere to the bell-glass by means of a small portion of shellac
or gum-lac. Screw on a metal ball or plate, to impart to it the
electricity you wish to test, which will be conveyed by the copper wire to
the gold leaf, and the latter will immediately move towards the plate
which has the opposite polarity. This electroscope is, beyond doubt, one
of the most delicate ever constructed, and is well adapted to show small
quantities of positive and negative electricity.

[Illustration: Fig. 91.]

"To ensure the susceptibility of electroscopes and electrometers placed
under bell-glasses, precautions should be taken to render the air they
contain as dry as possible, which may be effected by enclosing in a
suitable vessel a little melted chloride of calcium beneath the glass."

The galvanic pile employed in this electroscope is that invented by
Zamboni. "It differs from the common hydro-electric batteries principally
in this, that the presence of the electromotive liquid is dispensed with,
and that in its place is substituted some moist substance of low
conducting power, generally paper. The electromotors in these piles are
composed for the most part of Dutch gold (copper) and silver (zinc) paper
pressed one on the other, with their paper sides together, out of which
discs are cut with a diameter of from a quarter of an inch to an inch.
More powerful pairs of plates may be obtained by using only the silver
paper and smearing its paper side with a thin coat of honey, on which some
finely pulverized peroxide of manganese has been sprinkled, and all the
sides similarly coated are presented one way. Powerful pairs of plates may
also be made by pasting pure gold leaf on the paper side of zinc-paper.
These plates are then to be arranged, just as in the ordinary voltaic
pile, one above the other, so that the similar metallic surfaces may all
lie one way; press them tightly together; tie them with pretty stout silk
threads, and press them into a glass tube of convenient size. The metal
rims of the tubes, which must be well connected with the outermost pairs
of plates, form the poles of the pile, the negative pole being in the
extreme zinc surface, and the positive in the extreme copper or manganese
surface.

"The electromotive energy called into action in these dry piles is less
than that excited in the moist or hydro-electric piles, principally on
account of the imperfect conduction of the paper. The accumulation of
electricity at their poles also goes on less rapidly, and consequently the
electrical tension continues for a long while unaltered; whereas, in all
moist piles, even in the most constant of them, the tension is maintained,
comparatively speaking, for but a short time, on account of the chemical
action and decomposition of the electromotive fluid--causes of disturbance
which do not exist in the dry pile."[15]


=135. Thomson's Electrometer.=--Professor W. Thomson, of Glasgow, has
devised an atmospheric electrometer, which is likely to become eminently
successful, in the hands of skilful observers. It is mainly a torsion
balance combined with a Leyden-jar. The index is an aluminium needle
strung on a fine platinum wire, passing through its centre of gravity, and
stretched firmly between two points. The needle and wire are carefully
insulated from the greater part of the instrument, but are in metallic
communication with two small plates fixed beside the two ends of the
needle, and termed the repelling plates. A second pair of larger plates
face the repelling plates, on the opposite side of the needle, but
considerably farther from it. These plates are in connection with the
inner coating of a Leyden-jar, and are termed the attracting plates. The
whole instrument is enclosed in a metal cage, to protect the glass
Leyden-jar and the delicate needle.

The Leyden-jar should be charged when the instrument is used. Its effect
is two-fold: it increases greatly the sensibility of the instrument, and
enables the observer to distinguish between positive and negative
electrification.

The air inside the jar is kept dry by pumice-stone, slightly moistened
with sulphuric acid; by which means very perfect insulation is maintained.

Electrodes, or terminals, are brought outside the instrument, by which the
Leyden-jar can be charged, and the needle system connected with the body,
the electric state of which is to be tested.

For the purpose of testing the electric state of the atmosphere, the
instrument is provided with a conductor and support for a burning match,
or, preferably, with an arrangement termed a water-dropping collector; by
either of which means the electricity of the air is conveyed to the needle
system.

The needle abuts upon the repelling plates when not influenced by
electricity, in which position it is at zero. It can always be brought
back to zero by a torsion-head, turning one end of the platinum wire, but
insulated from it, and provided with a graduated circle, so that the
magnitude of the arc, that the torsion-head is moved through to bring the
needle to zero, measures the force tending to deflect it.

The action of the instrument is as follows:--The Leyden-jar is to be
highly charged, say negatively; and the repelling plates are to be
connected with the earth. The needle will then be deflected against a
stop, under the combined influence of attraction from the Leyden-jar, or
attracting plates, and repulsion from the repelling plates due to the
positive charge induced on the needle and its plates by the Leyden-jar
plates. The platinum wire must then be turned round by the torsion-head so
as to bring back the needle to zero; and the number of degrees of torsion
required will measure the force with which the needle is attracted. Next,
let the needle plates be disconnected from the earth, and connected with
the insulated body, the electric state of which is to be tested. In
testing the atmosphere, the conductor and lighted match, or water-dropping
apparatus, must be applied.

If the electricity of the body be positive, it will augment the positive
charge in the needle plates, induced by the Leyden-jar plates; and
consequently the needle will be more deflected than by the action of the
jar alone. If the electricity of the body be negative, it will tend to
neutralize the positive charge; and the needle will be less deflected.
Hence the kind of electricity present in the air becomes at once apparent,
without the necessity of an experimental test. The platinum wire must then
be turned till the needle is brought to zero, and the number of degrees
observed; which is a measure of the intensity of the electrification.

Any loss of charge from the Leyden-jar which may from time to time occur,
reducing the sensibility inconveniently, may be made good by additions
from a small electrophorus which accompanies the instrument.[16]

The instrument may be made self-recording by the aid of clockwork and
photography. To effect this, a clock gives motion to a cylinder, upon
which photographic paper is mounted. The needle of the electrometer is
made to carry a small reflector; and rays from a properly adjusted source
of light are thrown by the reflector, through a small opening, upon the
photographic paper. It is evident, that as the cylinder revolves, a trace
will be left upon the paper, showing the magnitude of, and variations in,
the deflection of the needle.


=136. Fundamental Facts regarding Atmospheric Electricity.=--The _general_
electrical condition of the atmosphere is _positive_ in relation to the
surface of the earth and ocean, becoming more and more positive as the
altitude increases. When the sky is overcast, and the clouds are moving in
different directions, it is subject to great and sudden variations,
changing rapidly from positive to negative, and the reverse. During fog,
rain, hail, sleet, snow, and thunderstorms, the electrical state of the
air undergoes many variations. The intensity of the electricity increases
with hot weather following a series of wet days, or of wet weather coming
after a continuance of dry days. The atmospheric electricity, in fact,
seems to depend for its intensity and kind upon the direction and
character of the prevailing wind, under ordinary circumstances. It has an
annual and a diurnal variation. There is a greater diurnal change of
tension in winter than in summer. By comparing observations from month to
month, a gradual increase of tension is perceived from July to February,
and a decrease from February to July. The intensity seems to vary with the
temperature. The diurnal variation exhibits two periods of greatest and
two of least intensity. In summer, the _maxima_ occur about 10 a.m. and 10
p.m.; the _minima_ about 2 a.m. and noon. In winter, the _maxima_ take
place near 10 a.m. and 8 p.m.; the _minima_ near 4 a.m. and 4 p.m.

The researches of Saussure, Beccaria, Crosse, Quetelet, Thompson, and
FitzRoy have tended to show that during the prevalence of polar currents
of air positive electricity is developed, and becomes more or less active
according to the greater or less coldness and strength of wind; but with
winds from the equatorial direction there is little evidence of sensitive
electricity, and when observable, it is of the negative kind. Storms and
gales of wind are generally attended, in places, with lightning and
thunder; and as the former are very often attributed to the conflict of
polar and equatorial winds, the difference of the electric tension of
these winds may account for the latter phenomena. It is not our intention
to enter upon the general consideration of thunderstorms; the facts which
we have given may be of service to the young observer; and finally, as it
is interesting to be able to judge of the locality of a thunderstorm, the
following simple rule will be of service, and sufficiently accurate:--Note
by a second's watch the number of seconds which elapse from the sight of
the lightning to the commencement of the thunder; divide them by five, and
the quotient will be the distance in miles. Thus, if thunder is heard ten
seconds after the lightning was seen, the distance from the seat of the
storm will be about two miles. The interval between the flash and the roll
has seldom been observed greater than seventy-two seconds.


=137. Lightning Conductors.=--"The line of danger, whether from the
burning or lifting power of lightning, is the line of strong and
obstructed currents of air, of the greatest aerial friction."[17] Trees,
church spires, wind-mills and other tall structures, obstruct the aerial
currents, and hence their exposure to danger. The highest objects of the
landscape, especially those that are nearest the thunder cloud, will
receive the lightning stroke. The more elevated the object, the more
likely is it to be struck. Of two or more objects, equally tall and near,
the lightning is invariably found to select the best conductor of
electricity, and even to make a circuitous path to get to it. Hence the
application and evident advantage of metallic rods, called _lightning
conductors_, attached to buildings and ships. A lightning conductor should
be pointed at top, and extend some feet above the highest part of the
edifice, or mast. It should be made of copper, which is a better
conducting medium than iron, and more durable, being less corrosive. It
must be unbroken throughout its length, and extend to the bottom of the
building, and even some distance into the ground, so as to conduct the
electricity into a well or moist soil. If it be connected with the lead
and iron work in the structure of the house, it will be all the better, as
affording a larger surface, and a readier means of exit for the fluid. In
a ship, the lower end of the conductor should be led into communication
with the hull, if of iron, and with the copper sheathing, if a wooden
vessel; so that, spread over a large surface, it may escape more readily
to the water.


=138. Precautions against Lightning.=--Experience seems to warrant the
assumption that any building or ship, fitted with a substantial lightning
conductor, is safe from danger during a thunderstorm. Should a house or
vessel be undefended by a conductor, it may be advisable to adopt a few
precautions against danger. In a house, the fire-place should be avoided,
because the lightning may enter by the chimney, its sooty lining being a
good conductor. "Through chimneys, lightning has a way into most houses;
and therefore, it is wise, by opening doors or windows, to give it a way
out. Wherever the aerial current is fiercest, there the danger is
greatest; and if we kept out of the way of currents or draughts, we keep
out of the way of the lightning."[18] Lightning evinces as it were a
preference for metallic substances, and will fly from place to place, even
out of the direct line of its passage to the earth, to enter such bodies.
It is therefore well to avoid, as much as possible, gildings, silvered
mirrors, and articles of metal. The best place is perhaps the middle of
the room, unless a draught passes, or a metallic lamp or chandelier should
be hanging from the ceiling. The neighbourhood of bad conductors, such as
glass windows, not being open, and on a thick bed of mattrasses, are safe
places. The quality of trees as lightning conductors is considered to
depend upon their height and moisture, those which are taller and
relatively more humid being struck in preference to their fellows;
therefore, it is unwise to seek shelter under tall and wet trees during a
thunderstorm. In the absence of any other shelter, it would be better to
lie down on the ground.




CHAPTER XV.

OZONE AND ITS INDICATORS.


=139. Nature of Ozone.=--During the action of a powerful electric machine,
and in the decomposition of water by the voltaic battery, a peculiar odour
is perceptible, which is considered to arise from the generation of a
substance to which the term ozone has been given, on account of its having
been first detected by smell, which, for a long time after its discovery,
was its only known characteristic. A similar odour is evolved by the
influence of phosphorus on moist air, and in other cases of slow
combustion. It is also traceable, by the smell, in air,--where a flash of
lightning has passed immediately before. Afterwards it was established
that the same element possessed an oxidising property. It was found to be
liberated at the oxygen electrode when water was decomposed by an electric
current; and has been regarded by some chemists as what is termed an
_allotropic_ form of oxygen, while others speak of it as oxygen in the
_nascent_ state, and some even regard it as intimately related to
chlorine. So various are the existing notions of the nature of this
obscure agent.

Its oxidising property affords a ready means for its detection, even when
the sense of smell completely fails. The methods of noting the presence
and measuring the amount of ozone present in the air, are very simple;
being the free exposure to the air, defended from rain and the direct rays
of the sun, of prepared test-papers. There are two kinds of test-papers.
One kind was invented by Dr. Schonbein, the original discoverer of ozone;
and the other, which is more generally approved, by Dr. Moffat.


=140. Schonbein's Ozonometer= consists of strips of paper, previously
saturated with a solution of starch and iodide of potassium, and dried.
The papers are suspended in a box, or otherwise properly exposed to the
air, for a given interval, as twenty-four hours. The presence of ozone is
shown by the test-paper acquiring a purple tint when momentarily immersed
in water. The amount is estimated by the depth of the tint, according to a
scale of ten tints furnished for the purpose, which are distinguished by
numbers from 1 to 10. The ozone decomposes the compound which iodine forms
with hydrogen, and, it is presumed, combines as oxygen with hydrogen,
while the iodine unites with the starch, giving the blue colour when
moist.


=141. Dr. Moffat's Ozonometer= consists of papers prepared in a somewhat
similar manner to Schonbein's; but they do not require immersion in water.
The presence of ozone is shown by a brown tint, and the amount by the
depth of tint according to a scale of ten tints, which is furnished with
each box of the papers.

Moffat's have the advantage of preserving their tint for years, if kept in
the dark, or between the leaves of a book; and are simpler to use.


[Illustration: Fig. 92.]

=142. Sir James Clark's Ozone Cage= (fig. 92), consists of two cylinders
of very fine wire gauze, one fitting into the other; the wire gauze being
of such a fineness as to permit the free ingress of air, at the same time
that it shuts out all light that would act injuriously on the test-paper,
which is suspended by a clip or hook attached to the upper part of the
inner cylinder.


=143. Distribution and Effects of Ozone.=--Mr. Glaisher has found that
"the amount of ozone at stations of low elevation is small; at stations of
high elevation, it is almost always present; and at other and intermediate
stations, it is generally so. The presence and amount of ozone would seem
to be graduated by the elevation, and to increase from the lowest to the
highest ground. The amount of ozone is less in towns than in the open
country at the same elevation; and less at inland than at sea-side
stations." It seems to abound most with winds from the sea, and to be most
prevalent where the air is considered the purest and most salubrious. This
may seem, says Admiral FitzRoy, in _The Weather Book_, to point to a
connection between ozone and chlorine gas, which is in and over sea-water,
and which _must_ be brought by any wind that blows from the sea. It
prevails more over the ocean and near it than over land, especially land
remote from the sea; and, says the Admiral, it affects the gastric juice,
improves digestion, and has a tanning effect. Dr. Daubeny, in his
_Lectures on Climate_, writes: "Its presence must have a sensible
influence upon the purity of the air, by removing from it foetid and
injurious organic effluvia. It is also quite possible that ozone may play
an important part in regulating the functions of the vegetable kingdom
likewise; and although it would be premature at present to speculate upon
its specific office, yet, for this reason alone, it may be well to note
the fact of its frequency, in conjunction with the different phases which
vegetation assumes, persuaded that no principle can be generally diffused
throughout nature, as appears to be the case, with this, without having
some important and appropriate use assigned for it to fulfil."


=144. Registering Ozonometer.=--Dr. E. Lancaster has contrived an
ozonometer, the object of which is to secure the constant registration of
ozone, so that the varying quantities present in the atmosphere may be
detected and registered. For this purpose, an inch of ozone paper passes
in each hour, by clock-work, beneath an opening in the cover of the
instrument.




CHAPTER XVI.

INSTRUMENTS NOT DESCRIBED IN THE PRECEDING CHAPTERS.


=145. Chemical Weather Glass.=--This curious instrument appears to have
been invented more than a hundred years ago, but the original maker is not
known. It is simply a glass vial about ten inches long and three quarters
of an inch in diameter, which is nearly filled, and hermetically sealed,
with the following mixture:--Two drachms of camphor, half a drachm of
nitrate of potassium, half a drachm of chlorate of ammonium, dissolved in
about two fluid ounces of absolute alcohol mixed with two ounces of
distilled water. All the ingredients should be as pure as possible, and
each vial filled separately. When the instruments are made in numbers and
filled from a common mixture, some get more than the due proportion of the
solid ingredients, and consequently such glasses do not exhibit that
uniformity of appearance and changes, that undoubtedly should accompany
similar influencing circumstances. It is in consequence of a want of
precision and fixed principle of manufacture, that these interesting
instruments are not properly appreciated, and more generally used.

The glass should be kept quite undisturbed, exposed to the north, and
shaded from the sun. Camphor is soluble in alcohol, but not in water,
while both water and alcohol have different solvent powers, according to
the temperature; hence, the solid ingredients being in excess for certain
conditions of solution, depending upon temperature chiefly, and perhaps
electricity and the action of light also, appear as crystals and disappear
with the various changes that occur in the weather.

The various appearances thus presented in the menstruum have been inferred
to prognosticate atmospheric changes. The following rules have been
deduced from careful study of the glass and weather:--

1. During cold weather, beautiful fern-like or feathery crystallization is
developed at the top, and sometimes even throughout the liquid. This is
the normal state of the glass during winter. The crystallization increases
with the coldness; and if the structure grows downward, the cold will
continue.

2. During warm and serene weather, the crystals dissolve, the upper and
greater part of the liquid becoming perfectly clear. This is the normal
state of the glass during summer. The less amount of crystallization, that
is, the greater the clear portion of the liquid (for there is always some
of the composition visible at the bottom), the greater the probability of
continued fine dry weather.

3. When the upper portion is clear, and flakes of the composition rise to
the top and aggregate, it is a sign of increasing wind and stormy
weather.

4. In cold weather, if the top of the liquid becomes thick and cloudy, it
denotes approaching rain.

5. In warm weather, if small crystals rise in the liquid, which still
maintains its clearness, rain may be expected.

6. Sharpness in the points and features of the fern-like structure of the
crystals, is a sign of fine weather; but when they begin to break up, and
are badly defined, unsettled weather may be expected.

Admiral FitzRoy, in _The Weather Book_, writes of this instrument as
follows:--"Since 1825, we have generally had some of these glasses, as
curiosities rather than otherwise; for nothing certain could be made of
their variations until lately, when it was fairly demonstrated that if
fixed undisturbed in free air, not exposed to radiation, fire, or sun, but
in the ordinary light of a well-ventilated room, or, _preferably_, in the
outer air, the chemical mixture in a so-called storm-glass varies in
character with the _direction_ of the wind--not its force, _specially_
(though it _may_ so vary in _appearance_, only from another cause,
_electrical tension_).

"As the atmospheric current veers toward, comes from, or is only
_approaching_ from the polar direction, this chemical mixture--if closely,
even microscopically watched--is found to grow like _fir_, _yew_, fern
leaves, or hoar-frost--or like crystallizations.

"As the wind, or great body of air, tends more from the _opposite_
quarter, the lines or spikes--all regular, hard, or crisp
features--gradually diminish, till they vanish.

"Before, and in a continued southerly wind, the mixture sinks slowly
downward in the vial, till it becomes shapeless, like melting white sugar.

"Before, or during the continuance of a northerly wind (polar current),
the crystallizations are beautiful (if the mixture is correct, the glass a
_fixture_, and duly _placed_); but the least motion of the liquid disturbs
them.

"When the main currents meet, and turn _toward the west_, making
_easterly_ winds, stars are more or less numerous, and the liquid dull, or
less clear. When, and while they _combine by the west_, making westerly
winds, the liquid is clear, and the crystallization well-defined, without
loose stars.

"While _any hard_ or _crisp_ features are visible below, above, or at the
top of the liquid (where they form for polar winds), there is _plus_
electricity in the air; a _mixture_ of polar current co-existing _in that
locality_ with the opposite, or southerly.

"When nothing but soft, melting, sugary substance is seen, the atmospheric
current (feeble or strong as it may be) is southerly with _minus_
electricity, unmixed with, and _uninfluenced_ by, the contrary wind.

"Repeated trials with a delicate galvanometer, applied to measure electric
tension in the air, have proved these facts, which are now found useful
for aiding, with the barometer and thermometer, in forecasting weather.

"Temperature affects the mixture much, but not solely; as many comparisons
of winter with summer changes of temperature have fully proved.

"A confused appearance of the mixture, with flaky spots, or stars, in
motion, and less clearness of the liquid, indicates south-easterly wind,
probably strong to a gale.

"Clearness of the liquid, with more or less perfect crystallizations,
accompanies a combination, or a contest, of the main currents, by the
_west_, and very remarkable these differences are,--the results of these
air currents acting on each other _from_ eastward, or from an entirely
opposite direction, the _west_.

"The glass should be wiped clean now and then,--and once or twice a year
the mixture should be disturbed, by inverting and gently shaking the glass
vial."


[Illustration: Fig. 93.]

=146. Leslie's Differential Thermometer.=--A glass tube having a large
bulb at each extremity, and bent twice at right angles, as represented in
figure 93, containing strong sulphuric acid tinged with carmine, and
supported at the centre by a wooden stand, constitutes the differential
thermometer as invented by Professor Leslie. The instrument is designed to
exhibit and measure small differences of temperature. Each leg of the
instrument is usually from three to six inches long, and the balls are
about four inches apart. The calibre of the legs is about 1/50 inch, not
more; the other part of the tube may be wider. The tube is filled with the
liquid, the bulbs contain air. When both bulbs are heated alike, each
scale indicates zero. The scale is divided so that the space between the
freezing and the boiling-points of water is equal to 1,000 parts. When one
bulb is heated more than the other, the difference of temperature is
delicately shown by the descent of the coloured fluid from the heated
ball. It is uninfluenced by changes in the temperature of the atmosphere;
hence it is admirably adapted for experiments of radiant heat. The theory
of the instrument is that gases expand equally for uniform increments of
heat.


=147. Rumford's Differential Thermometer= differs from that just described
in simply containing only a small bubble of liquid, which lies in the
centre of the tube, when both bulbs are similarly influenced. The bulbs
and other parts of the tube contain air. When one bulb is more heated than
the other, the bubble moves towards the one less heated; and the scale
attached to the horizontal part of the tube affords a measurement of the
difference of temperature.


[Illustration: Fig. 94.]

=148. Glaisher's Thermometer Stand.=--The thermometer stand consists of a
horizontal board as a base, of a vertical board projecting upwards from
one edge of the horizontal one, and of two parallel inclined boards,
separated from each other by blocks of three inches in thickness,
connected at the top with the vertical, and at the bottom with the
horizontal board, and the air passes freely about and between them all. To
the top of the inclined boards is connected a small projecting roof to
prevent the rain falling on the bulbs of the instrument, which are carried
on the face of the vertical board, with their bulbs projecting below it,
so that the air plays freely on the bulbs from all sides. The whole frame
revolves on an upright post firmly fixed to the ground, as shown in the
engraving, fig. 94; and in use, the inclined side is always turned towards
the sun.


=149. Thermometer Screen, for use at Sea.=--This screen, or shade, was
designed by Admiral FitzRoy, and has been in use for several years on
board H.M. vessels and many merchant-ships. It is about twenty-four inches
long by twelve wide and eight deep; having lattice-work sides, door, and
bottom; with perforation also at top, so contrived that the air has free
access to the interior, while the direct rays of the sun, rain, and sea
spray are effectually excluded from the thermometers mounted inside. There
is ample space for two thermometers placed side by side on brackets, at
least three inches from each other or any part of the exterior of the
screen. One thermometer should be fitted up as a "wet bulb" (see p. 105).
A small vessel of water can easily be fixed inside the screen so as to
retain its position and contents under the usual motions of the ship; and
by means of a piece of cotton-wick, or muslin rag tied round the bulb of
the thermometer and trailing into the cup of water, keep the bulb
constantly moist.

Self-registering thermometers should be protected by a similar screen. It
has been found that thermometric observations made at sea are not valuable
for scientific purposes unless the instruments have been duly protected by
such a screen.


=150. Anemoscope=, or Portable Wind Vane for travellers, with compass, bar
needle, &c., shows the direct course of the wind to half a point of the
compass.


[Illustration: Fig. 95.]

=151. Evaporating Dish, or Gauge= (fig. 95), for showing the amount of
evaporation from the earth's surface. This gauge consists of a brass
vessel, the area or evaporating surface of which is accurately determined;
and also a glass cylindrical measure, graduated into inches, tenths, and
hundredths of inches. In use, the evaporating gauge is nearly filled with
water, the quantity having been previously measured by means of the glass
cylinder; it is then placed out of doors, freely exposed to the action of
the atmosphere; after exposure, the water is again measured, and the
difference between the first and second measurement shows the amount of
evaporation that has taken place. If rain has fallen during the exposure
of the gauge, the quantity collected by it must be deducted from the
measured quantity; the amount is shown by the quantity of rain collected
in the rain gauge. The wire cage round the gauge is to prevent animals,
birds, &c., from drinking the water.


=152. Dr. Babington's Atmidometer=, or instrument for measuring the
evaporation from water, _ice or snow_, consists of an oblong hollow bulb
of glass or copper, beneath which and communicating with it by a
contracted neck is a second globular bulb, duly weighted with mercury or
shot. The upper bulb is surmounted by a small glass or metal stem, having
a scale graduated to grains and half-grains; on the top of which is fixed
horizontally a shallow metal pan. The bulbs are immersed in a vessel of
water having a circular hole in the cover through which the stem rises.
Distilled water is then gradually poured into the pan above, until the
zero of the stem sinks to a level with the cover of the vessel. Thus
adjusted, as the water in the pan evaporates, the stem ascends, and the
amount of evaporation is indicated in grains. This instrument affords a
means of measuring evaporation from _ice or snow_. An adjustment for
temperature is necessary.


=153. Cloud Reflector.=--At the International Exhibition 1862, Mr. J. T.
Goddard exhibited a cloud mirror, for ascertaining the direction in which
the clouds are moving.

The mirror is laid on a horizontal support near a window, and fastened so
that the point marked north may coincide with the south point of the
horizon,--the several points will consequently be reversed. The edge of a
conspicuous cloud is brought to the centre of the mirror, and the observer
keeps perfectly still until it passes off at the margin, where the true
point of the horizon _from which_ the clouds are coming can be read off.


=154. Sunshine Recorder.=--Mr. Goddard also exhibited an instrument which
he calls by this name. It works by letting the sun's rays pass through a
narrow slit, and fall on photographic paper wound round a barrel moved by
clock-work; the paper being changed daily, and the photographic impression
developed and fixed in the usual manner.[19]


155. SET OF PORTABLE INSTRUMENTS.

In a small box, 8 in. by 8 in. by 4 in., a complete set of meteorological
instruments have been packed. The lid of the box, by an ingenious
arrangement, is made to take off and hang up; on it are permanently fixed
for observation, a maximum and minimum, and a pair of dry and wet bulb
thermometers. The interior of the box contains a maximum thermometer in
vacuo for solar radiation, and a minimum for terrestrial purposes, one of
Negretti and Zambra's small pocket aneroid barometers, pedometer for
measuring distances, pocket compass, clinometer, and lastly a rain gauge.
This latter instrument consists of an accurately turned brass ring having
an india rubber body fastened to it to receive the rain, which is measured
off by a small graduated glass, also contained in the box. Gentlemen
travelling will find this compact observatory all that can be desired for
meteorological observations.


156. IMPLEMENTS.

The practical meteorologist will find the following articles very useful,
if not necessary. They scarcely require description; an enumeration will
therefore suffice:--_Weather Diagrams_, or prepared printed and ruled
forms, whereon to exhibit graphically the readings of the various
instruments to render their indications useful in foretelling weather,
&c.;--_Meteorological Registers_, or Record Books, for recording all
observations, and the deductions;--_Cloud Pictures_, by which the clouds
can be readily referred to their particular classification, very necessary
to the inexperienced and learners;--Cyclone Glasses, or Horns, outline
Maps with Wind-markers, are also useful, especially in forecasting
weather.


157. HYDROMETER.

A simple kind of hydrometer is very much used at sea, as "a sea-water
test;" and as the observations are usually recorded in a meteorological
register or the ship's log-book, it may not be altogether out of place to
give a description of it here.

[Illustration: Fig. 96.]

[Illustration: Fig. 97.]

It is constructed of glass. If made of brass, the corrosive action of
salt-water soon renders the instrument erroneous in its indications. The
shapes usually given to the instruments are shown in figs. 96 and 97. A
globular bulb is blown, and partly filled with mercury or small shot, to
make the instrument float steadily in a vertical position. From the neck
of the bulb the glass is expanded into an oval or a cylindrical shape, to
give the instrument sufficient volume for flotation; finally, it is
tapered off to a narrow upright stem which encloses an ivory scale, and is
closed at the top. The divisions on the scale read downward, so as to
measure the length of the stem which stands above the surface of any
liquid in which the hydrometer is floated. The denser the fluid, the
higher will the instrument rise; the rarer, the lower it will sink.

The indications depend upon the hydrostatic principle, that floating
bodies displace a quantity of the fluid which sustains them equal to their
own weight. According, therefore, as the specific gravities of fluids
differ from each other, so will vary the quantities of the fluids
displaced by the same body when floated successively in each.

The specific gravity of distilled water, at the temperature of 62 deg. _F_,
being taken as unity, the depth to which the instrument sinks when gently
immersed in such water is the zero of the scale. The graduations extend
from 0 to 40; the latter being the mark which will be level with the
surface when the instrument is placed in water, the specific gravity of
which is 1.040. In recording observations, the last two figures
only--being the figures on the scale--are written down. Sea-water usually
ranges from 1.020 to 1.036.

A small tin, copper, or glass cylinder is useful for containing the water
to be tested. It should be wider than the hydrometer, and always filled to
the brim. If fitted to a stand, which is supported by gimbals, it will be
very convenient. Water in a bucket, basin, or other wide vessel, acquires
motion at sea, and the eye cannot be brought low enough (on account of the
edges) to read off the scale accurately.

Errors of observation may occur with the hydrometer, if it be put into
water without being clean, or without being carefully wiped. The
instrument is extremely accurate if correctly used. It should be kept free
from contact with the sides of the vessel; and all dust, smears, or
greasiness, should be scrupulously avoided, by carefully wiping it with a
clean cloth before and after use.

Whenever the temperature of the water tested differs from 62 deg., a
correction to the reading is necessary, for the expansion or contraction
of the glass, as well as the water itself, in order to reduce all
observations to one generally adopted standard.

Negretti and Zambra's hydrometer, with thermometer in the stem, shows the
density and temperature in one instrument.

For the following Tables we are indebted to the kindness of Admiral
FitzRoy:--

TABLE for reducing observations made with a BRASS HYDROMETER, assuming the
linear expansion of brass to be 0.000009555 for 1 deg. F. The correction is
additive for all temperatures above 62 deg., and subtractive for temperatures
below 62 deg.

  +----------------------------------------------------------------------+
  |_t deg._|Correction.||_t deg._|Correction.||_t deg._|Correction.||_t deg._|Correction.|
  |----+-----------++----+-----------++----+-----------++----+-----------|
  | 32 | -0.0014   || 48 | -0.0010   || 64 | +0.0002   || 80 | +0.0020   |
  | 33 |   .0014   || 49 |   .0009   || 65 |   .0003   || 81 |   .0021   |
  | 34 |   .0014   || 50 |   .0009   || 66 |   .0004   || 82 |   .0023   |
  | 35 |   .0014   || 51 | -0.0008   || 67 |   .0005   || 83 |   .0024   |
  | 36 |   .0014   || 52 |   .0008   || 68 | +0.0006   || 84 |   .0026   |
  | 37 |   .0014   || 53 |   .0007   || 69 |   .0007   || 85 | +0.0027   |
  | 38 | -0.0014   || 54 |   .0006   || 70 |   .0008   || 86 |   .0029   |
  | 39 |   .0013   || 55 |   .0006   || 71 |   .0009   || 87 |   .0030   |
  | 40 |   .0013   || 56 | -0.0005   || 72 |   .0010   || 88 |   .0032   |
  | 41 |   .0013   || 57 |   .0004   || 73 |   .0011   || 89 |   .0033   |
  | 42 |   .0013   || 58 |   .0003   || 74 | +0.0013   || 90 | +0.0035   |
  | 43 |   .0012   || 59 |   .0003   || 75 |   .0014   || 91 |   .0036   |
  | 44 | -0.0012   || 60 |   .0002   || 76 |   .0015   || 92 |   .0038   |
  | 45 |   .0011   || 61 | -0.0001   || 77 |   .0016   || 93 |   .0040   |
  | 46 |   .0011   || 62 |  0.0000   || 78 |   .0018   || 94 |   .0041   |
  | 47 | -0.0010   || 63 | +0.0001   || 79 | +0.0019   || 95 | +0.0043   |
  +----------------------------------------------------------------------+

TABLE for reducing observations made with a GLASS HYDROMETER, assuming the
linear expansion of glass to be 0.00000463 for 1 deg. F. The correction is
additive for temperatures above 62 deg., and subtractive for temperatures
below 62 deg.

  +----------------------------------------------------------------------+
  |_t deg._|Correction.||_t deg._|Correction.||_t deg._|Correction.||_t deg._|Correction.|
  |----+-----------++----+-----------++----+-----------++----+-----------|
  | 32 | -0.0019   || 48 | -0.0012   || 64 | +0.0002   || 80 | +0.0023   |
  | 33 |   .0019   || 49 |   .0011   || 65 |   .0003   || 81 |   .0024   |
  | 34 |   .0018   || 50 |   .0011   || 66 |   .0004   || 82 |   .0026   |
  | 35 |   .0018   || 51 | -0.0010   || 67 |   .0005   || 83 |   .0027   |
  | 36 |   .0018   || 52 |   .0009   || 68 | +0.0007   || 84 |   .0029   |
  | 37 |   .0017   || 53 |   .0008   || 69 |   .0008   || 85 | +0.0031   |
  | 38 | -0.0017   || 54 |   .0008   || 70 |   .0009   || 86 |   .0032   |
  | 39 |   .0017   || 55 |   .0007   || 71 |   .0010   || 87 |   .0034   |
  | 40 |   .0016   || 56 | -0.0006   || 72 |   .0012   || 88 |   .0036   |
  | 41 |   .0016   || 57 |   .0005   || 73 |   .0013   || 89 |   .0037   |
  | 42 |   .0015   || 58 |   .0004   || 74 | +0.0014   || 90 | +0.0039   |
  | 43 |   .0015   || 59 |   .0003   || 75 |   .0016   || 91 |   .0041   |
  | 44 | -0.0014   || 60 |   .0002   || 76 |   .0017   || 92 |   .0042   |
  | 45 |   .0014   || 61 | -0.0001   || 77 |   .0018   || 93 |   .0044   |
  | 46 |   .0013   || 62 |  0.0000   || 78 |   .0020   || 94 |   .0046   |
  | 47 | -0.0013   || 63 | +0.0001   || 79 | +0.0021   || 95 | +0.0048   |
  +----------------------------------------------------------------------+


158. NEWMAN'S SELF-REGISTERING TIDE-GAUGE.

At places where the phenomena of the tides are of much maritime
importance, a continuous series of observations upon the rise and fall,
and times of change, is essentially necessary as a basis for the
construction of good tide tables; and as such observations should also be
accompanied with the registration of atmospheric phenomena, we have no
hesitation in inserting a description of an accurate self-registering
tide-gauge.

The tide-gauge, as shown in the illustration, consists of a cylinder, _A_,
which is made to revolve on its axis once in twenty-four hours by the
action of the clock, _B_. A chain, to which is attached the float, _D_,
passes over the wheel, _C_, and on the axis of this wheel, _C_ (in about
the middle of it) is a small toothed wheel, placed so as to be in contact
with a larger toothed wheel carrying a cylinder, _E_, over which passes
another smaller chain. This chain, passing along the upper surface of the
cylinder, _A_, and round a second cylinder, _F_, at its further end, is
acted on by a spring so as to be kept in a constant state of tension. In
the middle of this chain a small tube is fixed for carrying a pencil,
which, being gently pressed down by means of a small weight on the top of
it, performs the duty of marking on paper placed round the cylinder the
progress of the rise or fall of the tide as the cylinder revolves, and as
it is drawn by the chain forward or backward by the rise or fall of the
float. The paper is prepared with lines equidistant from each other, to
correspond with the hours of the clock, crossed by others showing the
number of feet of rise and fall.

[Illustration]

The cylinder while in action revolves from left to right to a spectator
facing the clock, and the pencil is carried horizontally along the top of
the cylinder; and the large wheel being made to revolve by the rise and
fall of the float, turns the wheel with the small cylinder, _E_,
attached to it. If the tide is _falling_, the small chain is wound round
the cylinder, _E_, and the pencil is drawn towards the large wheel; but if
the tide is _rising_, the small chain is wound on to the cylinder, _F_, by
means of the spring contained in it, which constantly keeps it in a state
of tension. Thus, by means of the rise and fall of the tide, a lateral
progress is given to the pencil, while the cylinder is made to revolve on
its axis by the clock, so that a line is traced on the paper showing the
exact state of the tide continuously, without further attention than is
necessary to change the paper once every day, and to keep the pencil
carefully pointed; or a metallic pencil may be used, which will require
little, if any, attention.

A good self-registering tide-gauge is a valuable and important acquisition
wherever tidal observations are required, and the only perfectly efficient
instrument of this kind is that invented by the late Mr. John Newman, of
Regent Street, London. It is now in action in several parts of the world,
silently and _faithfully_ performing its duty, requiring no other kind of
attention than that of a few minutes daily, and thus admitting the
employment of the person on any other service whose duty it would
otherwise have been to have registered the tide. It has done much by its
faithful records in contributing to the construction of good tide tables
for many places; for those unavoidable defects dependent on merely
watching the surface on a divided scale are set aside by it, all erroneous
conclusions excluded, and a true delineation of Nature's own making is
preserved by it for the theorist.




ADDENDA.


1. French barometers are graduated to millimetres. An English inch is
equal to 25.39954 millimetres. Hence, 30 inches on the English barometer
scales correspond to 762 millimetres on the French barometer scales.
Conversions from one scale to another can be effected by the following
formulae:--

  (1) Inches = millimetres divided by         25.39954
  (2) Millimetres = inches multiplied by      25.39954

Of course, a table of equivalent values should be drawn up and employed,
when a large number of observations are to be converted from one scale to
the other.


2. In Germany, barometers are sometimes graduated with old French inches
and lines,--the vernier generally indicating the tenth of a line.

OLD FRENCH LINEAL MEASURE.

                                              English Inches.
  1 douzieme, or point                        =  0.0074
  12 points              = 1 ligne            =  0.0888
  12 lignes              = 1 pouce            =  1.065765
  12 pouces              = 1 pied             = 12.7892
  1 pied                 = 324.7 millimetres.

"The Germans indicate inches by putting two accents after the number;
lines, by putting three accents; 27" 3'''.85, means 27 inches 3 lines 85
hundredths of a line; more frequently, they give the height in lines, and
the preceding number becomes 327'''.85."--_Kaemtz._


3. _Rule for finding Diameter of Bore of a Barometer Tube._

"If the maker has not taken care to measure the interior diameter
directly, it may be deduced from the exterior diameter. The exterior
diameter is first measured by calipers, and, by deducting from this
diameter 0.1 of an inch for tubes from .3 to .5 of an inch in external
diameter, we have an approximation to the interior diameter of the
tube."--_Kaemtz._


4. WIND SCALES.

  Sea Scale.       Wind.      Land Scale.
  ----------       -----      -----------
   0 to 3     =   Light     =   0 to 1
   3 "  5     =   Moderate  =   1 "  2
   5 "  7     =   Fresh     =   2 "  3
   7 "  8     =   Strong    =   3 "  4
   8 " 10     =   Heavy     =   4 "  5
  10 " 12     =   Violent   =   5 "  6


    Pressure in                  Velocity in
      Pounds      (Land Scale).     Miles
  (Avoirdupois)                   (Hourly).
  -------------    ---------     -----------
      1/2       =      1       =     10
       5        =      2       =     32
      10        =      3       =     45
      21        =      4       =     65
      26        =      5       =     72
      32        =      6       =     80


5. Letters to Denote the State of the Weather.

  _b_ denotes blue sky, whether with clear or hazy atmosphere.
  _c_    "    cloudy, that is detached opening clouds.
  _d_    "    drizzling rain.
  _f_    "    fog.
  _h_    "    hail.
  _l_    "    lightning.
  _m_    "    misty, or hazy so as to interrupt the view.
  _o_    "    overcast, gloomy, dull.
  _p_    "    passing showers.
  _q_    "    squally.
  _r_    "    rain.
  _s_    "    snow.
  _t_    "    thunder.
  _u_    "    ugly, threatening appearance of sky.
  _v_    "    unusual visibility of distant objects.
  _w_    "    wet, that is dew.

A letter repeated denotes much, as _r r_, heavy rain; _f f_, dense fog;
and a figure attached denotes duration in hours, as 14 _r_, 14 hours rain.

By the combination of these letters, all the ordinary phenomena of the
weather may be recorded with certainty and brevity.

EXAMPLES.--_b c_, blue sky with less proportion of cloud. 2 _r r l l t_,
heavy rain for two hours, with much lightning, and some thunder.

The above methods of recording the force of wind and state of weather
were originally proposed by Admiral Sir Francis Beaufort. They are now in
general use at sea, and by many observers on land.


6. Table of Expansion by Heat from 32 deg. to 212 deg. F.

  Platinum              0.0008842  of the length.
  Glass, Flint          0.0008117      "
    "    with Lead      0.0008622      "
  Brass                 0.0018708      "
  Mercury               0.0180180      "
  Water                 0.0433200, from 39 deg. to 212 deg.
  Alcohol               0.1100       "  32 deg. to 174 deg.
  Nitric Acid           0.1100
  Sulphuric Acid        0.0600


7. Table of Specific Gravity of Bodies at 32 deg. F. except water, which is
taken at 39 deg.4.

  Water                            1.000
  Alcohol, pure                    0.791
     "     proof                   0.916
  Mercury                         13.596
  Glass                      3 to  2.7
  Brass                    7.8 to  8.54
  Platinum                  21 to 22.00

Weight of a cubic foot of water, at the temperature of comparison, 62.425
lbs. avoirdupois.

The pound avoirdupois contains 7,000 grains.

Air is 813.67 times lighter than water.

The linear expansions are the mean values of the results of various
experimentalists. The specific gravities are as given in Professor
Rankine's _Applied Mechanics_.


8. Important Temperatures. Under the circumstances of--

                                                         deg.
  Water                          boiling at            212
  Mercury                         boils at             660
  Sulphuric Acid                     "                 590
  Oil of Turpentine                  "                 560
  Nitric Acid                        "                 242
  Alcohol                            "                 174
  A Saturated Solution of Salt       "                 218
  Vital Heat                                            96
  Olive Oil begins to solidify                          36
  Fresh Water freezes                                   32
  Sea Water freezes                                     28
  Mercury freezes                                      -39


9. TABLE OF METEOROLOGICAL ELEMENTS, FORMING EXPONENTS OF THE CLIMATE OF
LONDON.

  --------------------------------------------------------------------+
  1841     |Mean Height of Barometer, reduced to 32 deg. F., at the mean  |
   to      |    sea-level.                                            |
  1861.    |       +--------------------------------------------------|
           |       |Mean Monthly Range of Barometer.                  |
  Months.  |       |    +---------------------------------------------|
           |       |    |Mean of all the Highest Temperatures.        |
           |       |    |    +----------------------------------------|
           |       |    |    |Mean of all the Lowest Temperatures.    |
           |       |    |    |    +-----------------------------------|
           |       |    |    |    |Mean Temperature.                  |
           |       |    |    |    |    +------------------------------|
           |       |    |    |    |    |Mean Temperature of Dew-point.|
           |       |    |    |    |    |    +-------------------------|
           |       |    |    |    |    |    |Mean Degree of Humidity. |
           |       |    |    |    |    |    |  +----------------------|
           |       |    |    |    |    |    |  |Mean Number of  Rainy |
           |       |    |    |    |    |    |  |  Days.               |
           |       |    |    |    |    |    |  |   +------------------|
           |       |    |    |    |    |    |  |   |Average Rainfall. |
           |       |    |    |    |    |    |  |   |    +-------------|
           |       |    |    |    |    |    |  |   |    |Average      |
           |       |    |    |    |    |    |  |   |    |Amount of    |
           |       |    |    |    |    |    |  |   |    |Cloud (10=   |
           |       |    |    |    |    |    |  |   |    | overcast).  |
           |       |    |    |    |    |    |  |   |    |   +---------|
           |       |    |    |    |    |    |  |   |    |   |Prevalent|
           |       |    |    |    |    |    |  |   |    |   |Winds.   |
  ---------+-------+----+----+----+----+----+--+---+----+---+---------+
           |Inches.| In.|  deg.  |  deg.  |  deg.  |  deg.  |  |   | In.|   |         |
  ---------+-------+----+----+----+----+----+--+---+----+---+---------+
  January  | 29.932|1.44|43.2|33.7|38.3|35.4|89| 11| 1.8|7.7|W. to N. |
           |       |    |    |    |    |    |  |   |    |   |         |
  February | 29.962|1.22|44.7|33.2|38.4|34.4|85| 10| 1.6|7.4|S. to W. |
           |       |    |    |    |    |    |  |   |    |   |         |
  March    | 29.967|1.23|50.0|35.3|41.7|36.4|82| 10| 1.5|6.6|N. to E. |
           |       |    |    |    |    |    |  |   |    |   |         |
           |       |    |    |    |    |    |  |   |    |   |         |
  April    | 29.907|1.06|56.8|38.6|46.3|39.9|79| 11| 1.8|6.1|N. to E. |
           |       |    |    |    |    |    |  |   |    |   |         |
  May      | 29.931|1.02|64.4|44.2|52.8|45.5|76| 11| 2.1|6.1|S. to W. |
           |       |    |    |    |    |    |  |   |    |   |         |
  June     | 29.960|0.89|71.2|50.2|59.2|50.8|74| 11| 1.9|6.1|W. to N. |
           |       |    |    |    |    |    |  |   |    |   |         |
  July     | 29.970|0.79|73.8|53.2|61.9|53.9|76| 11| 2.7|6.9|W. to N. |
           |       |    |    |    |    |    |  |   |    |   |         |
  August   | 29.954|0.97|72.8|53.4|61.3|54.1|77| 11| 2.4|6.5|W. to N. |
           |       |    |    |    |    |    |  |   |    |   |         |
  September| 29.997|0.95|67.4|48.9|56.9|51.1|81| 12| 2.4|5.9|S. to W. |
           |       |    |    |    |    |    |  |   |    |   |         |
  October  | 29.860|1.33|58.3|43.7|50.2|46.0|87| 13| 2.8|6.9|S. to W. |
           |       |    |    |    |    |    |  |   |    |   |         |
  November | 29.929|1.53|49.3|37.7|43.4|40.1|89| 12| 2.4|7.2|  S.W.   |
           |       |    |    |    |    |    |  |   |    |   |         |
  December | 29.979|1.52|45.0|35.5|40.1|36.9|89| 12| 1.9|7.4|   W.    |
           |       |    |    |    |    |    |  |   |    |   |         |
  ---------+-------+----+----+----+----+----+--+---+----+---+---------+
  Year     | 29.946|1.16|58.0|42.3|49.2|43.7|82|133|25.3|6.7|   --    |
  ---------+-------+----+----+----+----+----+--+---+----+---+---------+
               1     2     3    4    5    6   7  8    9   10    11
  ---------------------------------------------------------------------

             +-----------------------------------------------------+
             |Sun above the Horizon on Middle Day.                 |
             |       +---------------------------------------------|
             |       |REMARKS.                                     |
    ---------+-------+---------------------------------------------|
             | Hours.|                                             |
    ---------+-------+---------------------------------------------|
    January  |  8-1/2|The majority of the nights are frosty.       |
             |       |                                             |
    February | 10    |10 frosty nights on the average.             |
             |       |                                             |
    March    | 12    |12 ditto   ditto     ditto.                  |
             |       |   Strong winds.                             |
             |       |                                             |
    April    | 14    | 6 ditto   ditto     ditto.                  |
             |       |                                             |
    May      | 15-1/2|Very rarely frost.                           |
             |       |                                             |
    June     | 16-1/2|Sun attains greatest North Declination, 21st.|
             |       |                                             |
    July     | 16    |                                             |
             |       |                                             |
    August   | 14-1/2|                                             |
             |       |                                             |
    September| 12-1/2|                                             |
             |       |                                             |
    October  | 10-1/2|A few frosty nights. Heavy gales.            |
             |       |                                             |
    November |  9    | 11 nights frosty.                           |
             |       |                                             |
    December |  8    |Sun attains greatest South Declination, 21st.|
             |       |                                             |
    ---------+-------+---------------------------------------------|
    Year     |   --  |                                             |
    ---------+-------+---------------------------------------------|
                 12               13                               |
    ---------------------------------------------------------------+

In the above Table, columns 1 to 10 are results obtained at the Royal
Observatory, Greenwich, by J. Glaisher, Esq., F.R.S. The data contained in
columns 2 and 10, are deduced from observations extending over the years
1841 to 1855 inclusive, and are copied from Edward Hughes' _Third Reading
Book_; the other columns are results of observations made during the
twenty years ending 1861. The rest of the information is from Luke
Howard's _Climate of London_.

These valuable data indicate the characteristics of the weather in each
month in the suburbs of London, and will be found tolerably accurate as
indications of weather, and serviceable as standards for comparisons of
observed results, at most places in England.




STANDARD WORKS ON METEOROLOGY

SUPPLIED BY NEGRETTI & ZAMBRA.

  THE WEATHER BOOK: A MANUAL OF PRACTICAL METEOROLOGY.
  By Vice-Admiral FITZROY, F.R.S., M.I.F., &c.
  _Price_, L0 15 6

  THE LAW OF STORMS,
  By H. W. DOVE, F.R.S.
  Translated by R. H. SCOTT, M.A.
  _Price_, L0 10 6

  L. F. KAEMTZ'S "COMPLETE COURSE OF METEOROLOGY,"
  Translated by C. V. WALKER, Esq.
  _Price_, L0 12 6

  PRACTICAL METEOROLOGY,
  By JOHN DREW, Ph.D., F.R.A.S.
  _Price_, L0 5 0

  HYGROMETRICAL TABLES,
  Adapted to the use of the Wet and Dry Bulb Thermometer,
  By JAMES GLAISHER, Esq., F.R.S.
  _Price_, L0 2 6

  TABLES OF THE CORRECTIONS FOR TEMPERATURES,
  To reduce observations to the 32 deg. Fahrenheit, for Barometers with brass
  scales extending from the cistern to the top of the mercurial column,
  By JAMES GLAISHER, Esq., F.R.S.
  _Price_, L0 1 0

  TABLE OF THE DIURNAL RANGE OF THE BAROMETER,
  By JAMES GLAISHER, Esq., F.R.S.
  _Price_, L0 0 6

  TABLES FOR CALCULATION OF HEIGHTS FROM OBSERVATIONS
  ON THE BOILING-POINT OF WATER,
  Adapted to the use of Negretti and Zambra's Boiling-point Apparatus.
  _Price_, L0 1 0

  A THERMOMETRICAL TABLE,
  ON THE SCALES OF FAHRENHEIT, REAUMUR, AND CENTIGRADE,
  By ALFRED S. TAYLOR, Esq., M.D., &c.
  _Price_, in Sheet, with explanatory Pamphlet, L0 1 6

  METEOROLOGICAL TABLES,
  For the reduction of Barometrical and Hygrometrical Observations,
  Determination of Heights by the Barometer and Boiling-point
  Thermometer, &c.
  By G. HARVEY SIMMONDS, M.B.M.S.
  _Price_, L0 2 6

  BAROMETER MANUAL,
  Compiled by Vice-Admiral FITZROY, F.R.S.,
  For the Board of Trade.
  _Price_, L0 0 6

  POCKET METEOROLOGICAL REGISTER AND NOTE-BOOK,
  With Diagrams for exhibiting the Fluctuations of Barometer, &c.
  Printed on metallic paper. _Price_, with Pencil, L0 3 0


  LONDON:
  PRINTED BY STRAHAN AND WILLIAMS,
  7 LAWRENCE LAND, CHEAPSIDE, E.C.




NEGRETTI & ZAMBRA'S

PATENT RECORDING AND DEEP-SEA THERMOMETER.[20]


This Thermometer differs from all other Registering or Recording
Thermometers in the following important particulars:--

I. The Thermometer contains only Mercury without any admixture of Alcohol
or other fluid.

II. It has no indices or springs, and its indications are by the column of
Mercury only.

III. It can be carried in any position, and cannot possibly be put out of
order except by actual breakage of the instrument.

And lastly, it will indicate and record the exact temperature at any hour
of the day or night, or the exact temperature at any depth of the sea,
irrespective of either warm or cold currents, or stratum through which the
Thermometer may have to pass in its descent or ascent, this last very
special quality renders this Thermometer superior for deep-sea
temperatures to any others; for those now being used in the "Challenger"
sounding expedition are liable to give erroneous indications owing to
their indices slipping, and otherwise getting deranged--(This was proved
by Messrs. Negretti and Zambra at a Meeting of the British Meteorological
Society,) and _under certain conditions of temperature_ it is not possible
by the old Thermometers to obtain true temperatures at certain depths
which might be required. _Annexed is a copy of a report to the Admiralty
from Captain G. S. Nares, of H.M.S. "Challenger," dated Melbourne, March
25th, 1874, which we have taken from NATURE, July 30th, 1874, proving
the assertion._

"In the report to the Admiralty of Capt. G. S. Nares, of H.M.S.
_Challenger_ dated Melbourne, March 25, 1874, Capt. Nares, speaking of the
temperature of the ocean, especially near the pack edge of the ice,
says:--'At a short distance from the pack, the surface water rose to 32 deg.,
but at a depth of 40 fathoms we always found the temperature to be 29 deg.;
this continued to 300 fathoms, the depth in which most of the icebergs
float, after which there is a stratum of slightly warmer water of 33 deg. or
34 deg. As the thermometers had to pass through these two belts of water
before reaching the bottom, the indices registered those temperatures, and
it was impossible to obtain the exact temperature of the bottom whilst
near the ice, but the observations made in lower latitudes show that it is
about 31 deg. More exact results could not have been obtained even had Mr.
Siemens's apparatus been on board.' It seems to us that the difficulty
mentioned is one which would certainly have been surmounted by Messrs.
Negretti and Zambra's new Recording Thermometers, a description of which
appeared in NATURE, vol. ix. p. 387; this being exactly one of the cases
to which this instrument is peculiarly adapted. We believe the inventors
and makers have greatly improved their Thermometer since our description
appeared, and no doubt means will be taken by the Admiralty to transmit
one to the _Challenger_."


DESCRIPTION OF THE DEEP-SEA RECORDING THERMOMETER.

In the first place, it must be observed that the bulb of the Thermometer
is protected so as to resist the pressure of the ocean, which varies
according to depth that of three thousand fathoms being something like
three tons pressure on the square inch. The manner of protecting the bulb
was invented by Messrs. Negretti and Zambra in 1857, and has been latterly
copied by other persons and brought out as a new invention. The manner of
protecting the bulb has been described by the late Admiral R. FitzRoy, in
the first number of Meteorological Papers, page 55, published July 5th,
1857, as follows:

    "Referring to the erroneous readings of all thermometers, consequent
    on their delicate bulbs being compressed by the great pressure of the
    ocean, he says:--'With a view to obviate this failing, Messrs.
    Negretti and Zambra undertook to make a case for the weak bulbs, which
    should transmit temperature, but resist pressure. Accordingly a tube
    of thick glass is sealed outside the delicate bulb, between which and
    the casing is a space all round, which is nearly filled with mercury.
    The small space not so filled is a vacuum, into which the mercury can
    be expanded, or forced by heat or mechanical compression, without
    doing injury to or even compressing the inner or much more delicate
    bulb.'"

[Illustration: Fig. 1.]

The construction of this instrument for deep-sea temperatures is as
follows:--

    In shape it is like a syphon with parallel legs, all in one piece and
    having a continuous communication, as in the annexed figure. The scale
    of the Thermometer is pivoted on a centre and being attached in a
    perpendicular position to a simple apparatus (which will be presently
    described), is lowered to any depth that may be desired. In its
    descent the Thermometer acts as an ordinary instrument, the mercury
    rising or falling according to the temperature of the stratum through
    which it passes; but so soon as the descent ceases, and a reverse
    motion is given to the line, so as to pull the Thermometer towards the
    surface, the instrument turns once on its centre, first bulb
    uppermost, and afterwards bulb downwards. This causes the mercury,
    which was in the left-hand column, first to pass into the dilated
    syphon bend at the top, and thence into the right-hand tube, where it
    remains, indicating on a graduated scale the exact temperature at the
    time it was turned over. The woodcut, Fig. 1, shows the position of
    the mercury _after_ the instrument has been thus turned on its centre.
    A is the bulb; B the outer coating or protecting cylinder; C is the
    space of rarefied air, which is reduced if the outer casing be
    compressed; D is a small glass plug on the principle of Negretti and
    Zambra's Patent Maximum Thermometer, which cuts off, in the moment of
    turning, the mercury in the tube from that of the bulb, thereby
    ensuring that none but the mercury in the tube can be transferred into
    the indicating column; E is an enlargement made in the bend so as to
    enable the mercury to pass quickly from one tube to another in
    revolving; and F is the indicating tube or Thermometer proper. In its
    action, as soon as the Thermometer is put in motion, and immediately
    the tube has acquired a slightly oblique position, the mercury breaks
    off at the point D, runs into the curved and enlarged portion E, and
    eventually falls into the tube F when this tube resumes its original
    perpendicular position.

The contrivance for turning the Thermometer over may be described as a
frame with a vertical propeller; to this frame the instrument is pivoted.
On its descent through the water the propeller is lifted out of gear and
revolves freely on its axis; but so soon as the instrument is pulled
towards the surface the propeller falls into gear and revolves in the
contrary direction, turning the Thermometer over once, and then becoming
locked and immovable.


_Directions for adjusting the Thermometer previous to its being lowered in
the Sea._

    I. The mercury must all be in the left-hand column.

    II. The short peg at the back of the thermometer must be in front of
    the stop plate S +; in order to effect this, pull the knob which stops
    the Thermometer, and slightly turn the propeller, to make the
    Thermometer advance sufficiently to escape the stop plate.

Negretti & Zambra's Patent Atmospheric Recording Thermometer, Fig. 3,
differs from the Deep-sea Thermometer by its not having the double or
protected bulb, it not being required for resisting pressures. In this
case the instrument is turned over by a simple clock movement, which can
be set to any hour it may be desirable; the Thermometer is fixed on the
clock, and when the hand arrives at the hour determined upon, and to which
the clock is set as in setting an alarum clock, a spring is released and
the Thermometer turns over as before described.

[Illustration: Fig. 2.]

[Illustration: Fig. 3.]

Messrs. Negretti and Zambra have arranged a Wet and Dry Bulb Hygrometer
upon the same plan.




NEGRETTI & ZAMBRA'S PRICE LIST OF STANDARD METEOROLOGICAL AND OTHER
PHILOSOPHICAL INSTRUMENTS.

_The marginal figures in this List and the numbers of the wood engravings
refer to paragraphs in "Negretti & Zambra's Treatise on Meteorological
Instruments."_


                                                                  L  s. d.

  4 =Standard Barometers=, Fortin's arrangement, as Fig. 3
  with mahogany board                                             8   8  0

      Ditto    ditto with Millemetre and English scales           9   9  0

      Ditto    ditto with tube, 0.45 internal diameter and
                     millimetre scale                            10  10  0

  =Observatory Standard Barometers=, extra large tubes and
  cisterns                                          L25  0  0    35   0  0

      Ditto    ditto arranged for observations being taken
                     by the Cathetometer                         18  18  0

  =Cathetometer=, for use with above                             21   0  0

  9 =Self Compensating Standard Barometer=, Fig. 6               20   0  0

  10 =Standard Barometer=, with electrical adjustment            15  15  0

  11 =Pediment Barometers=, Fig 7                    L1  1  0     2   2  0

     Ditto      ditto     Fig. 8                     L3  3  0     3  10  0

     Ditto      ditto     Fig. 9                     L4 10  0     5  10  0

     Ditto      ditto     Fig. 10                                 8  10  0

     Ditto      ditto     ditto handsome carved mountings,
     in mahogany, oak, or walnut wood    L8  8  0   L10 10  0    12  12  0

  14 =FitzRoy's Storm or Sea Coast Fishery Barometer=, Fig. 12    5   5  0

     Ditto    ditto with two verniers                             6   6  0

     Ditto    ditto mounted in ornamental carved frames, oak,
     walnut, or mahogany                             L6 10  0     8   8  0

  19 =Marine Barometers=, ordinary forms, Figs. 13 and 14
                                         L2  2s.     L2 10s.      3   3  0

     Ditto    ditto   Best mounted                   L5  5s.      6   6  0

  20 =The Board of Trade or Kew Marine Barometer=, Fig. 15,
                                         L4  4s.     L5  5s.      6   6  0

  22 =Negretti and Zambra's FitzRoy Marine or Gun Barometer=,
       Fig. 16, with N. and Z.'s Patent Porcelain Scales, as
       used in Her Majesty's Navy                                 5  10  0

     Extra Tube for ditto                                         1  15  0

  25 =Negretti and Zambra's Farmer's Barometer or Domestic
  Weather Glass=, Fig. 17                                         2  10  0

  28 =Negretti and Zambra's Miner's Barometers=
                                         L1  1s.     L2  2s.      3   3  0

  31 =Dial or Wheel Barometers=, Figs. 18, 19, 20, 21
                                         L3  3s.     L4  4s.      5   5  0

     Ditto  ditto  in carved ornamental mountings
                             L5 10s.     L6  6s.     L8  8s.     10  10  0

     Ditto  ditto  rosewood, inlaid with pearl or metal. Made
     to order, Figs. 22 and 23. Price varying with size, &c.

  37 =Gay Lussac's Syphon Tube Mountain Barometer=   L6  6  0     8   8  0

  32 =Standard Syphon Barometer=, Gay Lussac's arrangement,
     Fig. 24                                                      5   5  0

  38 =Negretti and Zambra's Standard Mountain Barometer=, with
     Fortin's cistern, with tripod stand and travelling case,
     Fig. 30                                                     10  10  0

  34 =Barograph, or Self-registering Barometer=, with syphon
     mercurial tube. Negretti and Zambra's improved arrangement,
     Fig. 26                                         18 18  0    25   0  0

  =Negretti and Zambra's Self-recording Aneroid Barometer=,
  with =Clock=                                                   22   0  0


  48. =ANEROID BAROMETERS.=

  =Aneroid Barometers,= with card dials 4-1/2 inches diameter,
  best quality.                                                   2  10  0

    Ditto    ditto      with silvered metal dial                  3   0  0

    Ditto    ditto      with ditto and thermometer                3  10  0

    Ditto    ditto         ditto   with corrected scale, as
    supplied by Negretti and Zambra to the Royal Navy             5   5  0

  =Aneroid Barometers=, with elegantly-chased dials               4   4  0

    Ditto    ditto      with raised ring on dial                  5   5  0

    Ditto    ditto         ditto    with thermometer              6   6  0

  =Aneroid Barometer=, for altitude measurements with revolving
  ring, carrying index, range of scale 20,000 feet 4-1/2 inches
  diameter, with magnifier                                        8   8  0


  =POCKET ANEROID BAROMETERS.= Fig. 34.

  49 =Pocket Aneroid Barometer=, 2-3/4 inches diameter, with
     silvered metal scale                                         3   3  0

     Ditto   ditto  for measuring altitudes to 10,000 feet
     compensated for temperature, in leather case                 5   5  0

     Ditto   ditto  ditto to 20,000 feet, with magnifier          6   6  0


  50 =WATCH-SIZE ANEROID BAROMETERS= in gilt metal cases (see figure 35.)

  =Watch-Size Aneroid Barometer=, weather range      L3  3  0     4   4  0

  Ditto      ditto  of best construction, extra thin, for
  meteorological observations or altitude measurements to
  10,000 feet                                                     5   5  0

  Ditto      ditto  ditto  to 20,000 feet, compensated for
  temperature                                                     6   6  0

  Either of the above Watch-size Barometers may be had in Stout
  Silver Cases at a cost of L2 2s. extra

  _Watch-size Aneroid Barometers in Solid Gold, highly-finished cases.
  L15 15s. to L21._

  Table Stands for Aneroid Barometers of Carved Oak or other woods,
  10s. 6d., 25s., 35s., to L5 5s.

  =Ships' Aneroid Barometers=, in suitable mountings L2 10s. L3 3s.
  L5 5s. L6 6s.


  47 =Sympiesometer=, for Ship use                   L3  3  0     4  10  0

     Ditto     ditto  Pocket form, Fig. 32                        4   4  0

  The Sympiesometer is now rarely used, the Aneroid Barometer being
  found equally sensitive and less liable to derangement.


  56 =Independent Standard Thermometers=, Fig. 36                 5   5  0

  57 =Standard Thermometers=, for Boiling Point Apparatus         1  10  0

  =Chemists' or Brewers' Standard Reference Thermometers=
                                                     L1  1s.      2   2  0

  47 =Chemical Thermometers=, divided on the stem. Fig. 48.
                                                    10s. 6d.      0  15  0

  =Chemical Thermometers=, Boxwood Scale  7s.  6d.  10s. 6d.      0  12  6

  64 =Thermometers on Boxwood Scales=, Fig. 37.
                         1s.   1s.  6d.   2s.  6d.   3s. 6d.      0   4  6

     Ditto   ditto   larger sizes                    7s. 6d.      0  12  6

     Ditto   ditto   Engraved glass scales, Fig. 39
                                    15s.   L1  1s.   L1  5s.      1  10  0


  =POCKET THERMOMETERS, IN VARIOUS MOUNTINGS.=

  Fig. 38   10s. 6d.    Fig. 40   10s. 6d. 15s.
  Fig. 41    5s. 6d.   8s. 6d.   12s. 6d.

  63 =Thermometers of extreme Sensitiveness=, 15s.   L1 10s.      2   2  0


  =Drawing Room or Mantel Thermometers=, various mountings,

  Figs. 42 and 43.  12s. 6d.  15s.  L1 1s.  L1 10s.  L2  2s.      2  10  0

  =Bracket Window Thermometers=, Fig. 46
                                  12s. 6d.    15s.   L1  1s.      1  10  0

  =Bath Thermometers=, Figs. 44                     7s.  6d.      0  15  0

  66 =Sugar Boiling Thermometers=           L1 12s.  L2  2s.      3   3  0

  67 =Earth Thermometers=, Fig. 51                   L1 10s.      2   2  0

     Hot Bed      Ditto                    12s. 6d.  L1  5s.      1  10  0

  68 =Marine Thermometer=, Fig. 52          7s. 6d.  8s. 6d.      0  10  6

  65 =Super Heated or Steam Pressure Thermometers=, Fig. 74,
     Figs. 49 and 50               L1 5s.   L1 10s.  L2  2s.      2  10  0


  =SELF-REGISTERING THERMOMETERS FOR HEAT.=

  72 =Negretti and Zambra's Patent Standard Maximum
     Self-Registering Thermometer=,[21] Fig. 54                   1   1  0

  72 =Negretti and Zambra's Patent Maximum Thermometer=, on
  boxwood scale                                                   0  10  6

     Ditto,  ditto,  on Negretti and Zambra's Patent Solid
     Porcelain or Metal Scales on oak mounting                    0  12  6

  70 =Rutherford's Maximum Thermometer=, on boxwood or metal
     scale, with steel index                5s. 6d.  7s. 6d.      0  10  6

  71 =Phillip's Maximum Thermometer=, on boxwood or metal
     scale, with air index                  7s. 6d.  10  6        0  12  6


  =SELF-REGISTERING THERMOMETERS FOR COLD.=

  73 =Negretti and Zambra's Standard Minimum Self-Registering
     Thermometer=, Fig. 55                                        1   1  0

  73 =Rutherford's Minimum Thermometer=, on boxwood or metal scale
                                   3s. 6d.    5s. 6d.   7s. 6d.   0  10  6

  73 =Rutherford's Minimum Thermometer=, on Negretti and Zambra's
     Patent solid porcelain scale                      10s. 6d.   0  12  6

     Ditto, on Negretti and Zambra's porcelain or metal scales
     and oak mounting                                             0  12  6

  74 =Negretti and Zambra's Horticultural Self-Registering
     Thermometer.= The scale is made of stout zinc, enclosing
     the tube; the figures and divisions are boldly marked for
     quickly and easily reading the indications, Fig. 56          0   3  6


  83 =Negretti and Zambra's Patent Solar Radiation Thermometer=,
     Fig. 63                                                      1   5  0

  84 Ditto,   ditto,   ditto, in vacuo, Fig. 64                   1  10  0

     Ditto,   ditto,   ditto, improved form, with test gauge      2   2  0

  85 =Negretti and Zambra's Terrestrial Radiation Thermometer=    1   5  0

  Brass Stands for above, Fig. 65                                 0   5  0

  76 and 77 =Negretti and Zambra's Patent Mercurial Minimum
     Thermometers=                                   L2 10s.      2   2  0

  81 =Maxima and Minima Thermometers=, on Sixe's arrangement,
     Fig. 62, various forms of mounting
                                  12s. 6d.    14s.    21s. 30s.   2   2  0

  =Pocket Maxima and Minima Thermometers=, Negretti and Zambra's
  Patent, in convenient cases                        L2  2s.      2  10  0

  89 =Deep Sea Registering Thermometer=, with Negretti and
     Zambra's improved protected bulb, in copper cylinder,
     Fig. 69.                                                     2  10  0

  89[21] =Negretti and Zambra's Improved Deep Sea Thermometer=,
     with vulcanite mountings, in copper cylinder, with door,
     small size                                                   2   5  0

  90 =Negretti and Zambra's Patent Recording Deep Sea
     Thermometer=                                                10  10  0

  91 Ditto,   ditto,   ditto   =Recording Thermometer=            4   4  0

  92 Ditto,   ditto,   ditto   =Hygrometer=                       6   6  0

  93 =Improved Boiling Point Mountain Thermometer=, or
     Hypsometric Apparatus, with Tables, Figs. 72 and 73, in
     leather case with strap                                      5   5  0

     Extra Thermometer for Ditto                                  1  10  0

  106 =Negretti and Zambra's Standard Wet and Dry Bulb
      Hygrometer=, Fig. 79                                        2   2  0

      Wet and Dry Bulb Hygrometers, various mountings
                                   30s.   25s.   21s.   14s.      0  10  6

      Pocket Hygrometers, in box                     L2  2s.      2  10  0

  103 =Daniell's Hygrometer=, Fig. 77                             3   3  0

  104 =Regnault's Hygrometer=, Fig. 78               L3 10s.      5   5  0

      Aspirator for Ditto                            L1 15s.      2  15  0


  110 =Howard's Rain Gauge=, has a 5-inch copper Funnel, with
      turned brass rim fitted to a stout stone-ware or glass
      bottle, with a graduated glass measure, divided to 100ths
      of an inch                                                  0  10  6

      =Symons' Portable Rain Gauge=, (5-inch) with graduated
      glass measure, japanned tin                                 0  10  6

      Ditto   ditto   in stout copper                             0  15  0

  111 =Glaisher's Rain Gauge=, the receiving surface is 8-inches
      diameter, of stout japanned metal, with graduated glass
      measure, Fig. 84                                            1   1  0

      Ditto   ditto,  of stout copper                             1  10  0

      Receiving Pots for ditto, extra 2s. and 3s. 6d.

  113 =Rain Gauge=, having a receiving surface of 12 inches
      diameter, and graduated glass gauge tube, divided to
      hundredths of an inch, in japanned metal, with brass tap    2  10  0

      Ditto   ditto, Fig. 85, in copper                           3  10  0

      Ditto   ditto, with sliding rod instead of graduated tube,
      japanned tin                                                2   2  0

      =Rain Gauges=, of any form or area made to order, with suitable
      measuring glasses.


  123 =Lind's Anemometer=, Fig. 86                                2   2  0

  125 =Robinson's Anemometer=, Fig. 87                            3   3  0

      Ditto   ditto,   Improved arrangement          L4 10s.      5  15  0

      Ditto   ditto,   with clutch movement, Fig. 88              6  15  0

      =Negretti and Zambra's Improved Air Meter=, of extreme
      sensitiveness, very portable                                4   4  0

      Large Air Meters made to order.

  127 =Osler's Self-Registering Anemometer and Rain Gauge=,
      Fig. 89                                            L84 to 150   0  0

  128 =Berkley's Anemometers= fitted up to order, _to suit the
      Observatory_.

  131 =Gold Leaf Electrometer=, Fig. 90                           1   1  0

  133 =Peltier's Electrometer=                                    4   4  0

  134 =Bohnenberger's Electroscope=, Fig. 91                      8   8  0

  135 =Thompson's Electrometer=, to order

      =Lightning Conductors= fitted up to order.

  142 =Ozone Cage=, Fig. 92                                       0  18  0

      Ditto  ditto, copper                                        1   5  0

  146 =Leslie's Differential Thermometer=, Fig. 93    L1 10s.     2   2  0

  148 =Thermometer Stand (Glaisher's)=                            3   3  0

  149 =Thermometer Screen= for Sea use                            3   3  0

  150 =Anemoscope=, or Portable Vane, Fig. 94                     2   5  0

  151 =Evaporating Dish=, Fig. 95                                 1   2  6

  157 =Sea Water Hydrometers=, Board of Trade Marine, Figs. 96
      and 97                                                      0   5  6

  158 =Newman's Self-Registering Tide Gauge=, Fig. 158, fitted
      to the Building to order                              From 50   0  0


  _Further Information as to Price, &c., will be found in_
  NEGRETTI & ZAMBRA'S ENCYCLOPAEDIC CATALOGUE OF
  MATHEMATICAL, PHILOSOPHICAL, OPTICAL, PHOTOGRAPHIC,
  AND STANDARD METEOROLOGICAL INSTRUMENTS,

  _Containing very numerous Comparative Tables of Reference,
  and Illustrated by upwards of_

  ELEVEN HUNDRED ENGRAVINGS.

  Royal 8vo. Cloth, Gilt Lettered--Price 5s. 6d.




FOOTNOTES:

[1] Second Number of "Meteorological Papers," issued by the Board of
Trade.

[2] With reference to these barometers, we have received the subjoined
testimonial, with permission to use it as we please.

    "_Meteorologic Office, 12th June, 1863._

    "MESSRS. NEGRETTI & ZAMBRA,

    "The barometers which you have lately supplied to Her Majesty's ships
    through this Office are much approved, being good for general service,
    afloat or on land.

    "(Signed)       R. FITZROY."

[3] _Vide_ C. Daubeny, F.R.S., "On Climate."

[4] _Vide_ Report of the British Association, 1862.

[5] See page 42 for the Tables.

[6] The quotations in this section are from Tyndall's _Heat considered as
a Mode of Motion_.

[7] Dr. Daubeny, F.R.S., _On Climate_.

[8] Leslie _On the Relations of Air, Heat, and Moisture_.

[9] Tyndall's _Heat considered as a Mode of Motion_.

[10] Vide _Horological Journal_, Vol. V.

[11] _Hygrometrical Tables_, by J. Glaisher, Esq., F.R.S.

[12] Vide _Report of the British Association_, 1862. It may be added, for
the information of those who are about to commence observing, that Mr.
Symons, of Camden Road Villas, London, is desirous of securing returns of
rain-fall from as many stations as possible, in order to render more
complete his annual reports to the British Association.

[13] Luke Howard's _Climate of London_.

[14] Vide _Third Number of Meteorological Papers_, issued by the Board of
Trade.

[15] _Elements of Physics_, by C. F. Peschel.

[16] This description is modified from that in Report of the Jurors for
Class XIII. International Exhibition, 1862.

[17] _All the Year Round_, No. 224.

[18] _All the Year Round_, No. 224.

[19] Vide _Jurors' Reports_.

[20] See also page 90 of this Treatise.

[21] These Instruments are the only Maximum Thermometers that can be
recommended, as unless they be broken, they cannot be put out of
adjustment. Fully described under the head of Standard Maximum
Thermometers in our large Catalogue, and page 72 of our _Treatise on
Meteorological Instruments_.






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