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