Meteorology; or, Weather ExplainedM'Pherson, J. G. (John Gordon)
Science
Meteorology; or, Weather Explained
M'Pherson, J. G. (John Gordon)
Meteorology
One of the heaviest rainfalls yet recorded in Great Britain was about
2-1/4 inches in forty minutes at Lednathie, Forfarshire, in 1887. Now 1
inch deep of rain means 100 tons on an imperial acre; so the amount of
water falling on a field during that short time is simply startling. The
heaviest fall for one day was at Ben Nevis Observatory, being fully 7-1/4
inches in 1890. In other parts of the world this is far exceeded. In one
day at Brownsville, Texas, nearly 13 inches fell in 1886. On the Khasi
hills, India, 30 inches on each of five successive days were registered.
At Gibraltar, 33 inches were recorded in twenty-six hours.
The heaviest rainfalls of the globe are occasioned by the winds that have
swept over the most extensive ocean-areas in the tropics. On the summer
winds the rainfall of India mainly depends; when this fails, there is most
distressing drought. Reservoirs are being erected to meet emergencies.
From Dr. Buchan's statistics it is found that the annual rainfall at
Mahabaleshwar is 263 inches; at Sandoway 214; and at Cherra-pungi 472
inches, the largest known rainfall anywhere on the globe. Over a large
part of the Highlands of Scotland more than 80 inches fall annually, while
in some of the best agricultural districts there it does not exceed 30
inches.
Of all meteorological phenomena, rainfall is the most variable and
uncertain. Symons gives as tentative results from twenty years'
observations in London--(1) In winter, the nights are wetter than the
days; (2) in spring and autumn, there is not much difference; (3) in
summer, nearly half as much again by day as by night.
The wearisomeness of statistics may be here relieved by a short
consideration of the _splash_ of a drop of rain. Watching the
drop-splashes on a rainy day in the outskirts of the city, when unable to
get out, I brought to my recollection the marvellous series of experiments
made by Professor A. M. Worthington in connection with these phenomena. Of
course, I could not see to proper advantage the formation of the
splashes, as the heavy raindrops fell into these tiny lakes on the quiet
road. There is not the effect of the huge thunder-drops in a stream or
pool. The building up of the bubbles is not here perfect, for the domes
fail to close, nor are the emergent columns visible to the naked eye. It
is a pity; for R. L. Stevenson once wrote of them in his delightful
"Inland Voyage," when he canoed in the Belgian canals, as thrown up by the
rain into "an infinity of little crystal fountains."
Beautiful is this effect if one is under shelter, every dome seeming quite
different in contour and individuality from all the rest. But terrible is
it when out fishing on Loch Earn, even with the good-humoured old Admiral,
when the heavy thunder-drops splash up the crystal water, and one gets
soaked to the skin, sportsman-like despising an umbrella.
Public-domain text, read in full here on John Shaqi.
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