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
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.
Public-domain text, read in full here on John Shaqi.
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