A Treatise on Meteorological Instruments: Explanatory of Their Scientific Principles, Method of Construction, and Practical UtilityNegretti, Enrico Angelo Lodovico
Science
A Treatise on Meteorological Instruments: Explanatory of Their Scientific Principles, Method of Construction, and Practical Utility
Negretti, Enrico Angelo Lodovico
Meteorological instruments; Meteorology; Scientific apparatus and instruments
=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.]
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