The Rain Cloud: or, An Account of the Nature, Properties, Dangers and Uses of Rain in Various Parts of the WorldTomlinson, Charles
Science
The Rain Cloud: or, An Account of the Nature, Properties, Dangers and Uses of Rain in Various Parts of the World
Tomlinson, Charles
Clouds; Rain and rainfall; Weather
The annual quantity of rain decreases from the equator to the poles, as
appears from the following table, which gives the name of the station,
its latitude, and the average annual number of inches of rain:—
Coast of Malabar lat. 11° 30′ N. 135½ inches.
At Grenada, Antilles 12° 126
At Cape François, St. 19° 46′ 120
Domingo
At Calcutta 22° 23′ 81
At Rome 41° 54′ 39
In England 50 to 55° 31
At St. Petersburgh 59° 16′ 16
At Uleaborg 65° 30′ 13½
The number of rainy days, on the contrary, increases from the equator to
the poles.
From 12° to 43° N. lat.—the number of rainy days in the 78
year amounts to
From 43° to 46° 103
From 46° to 50° 134
From 50° to 60° 161
The greatest depth of rain which falls in the Indian ocean is during the
time when the periodical winds, called the _monsoons_, change their
direction. When the winds blow directly in-shore the rains are very
abundant, so much so that, after a continuance of twenty-four hours, the
surface of the sea has been covered with a stratum of fresh water, good
enough for drinking, and ships have actually filled their casks from it.
Colonel Sykes observes, that the deluge-like character of a monsoon in
the Ghàts of Western India, is attested by the annual amount of 302¼
inches, at Malcolmpait, on the Mahabuleshwar Hills.
A great depth of rain in a short time has occasionally been witnessed in
Europe. At Genoa, on the 25th of October, 1822, a depth of thirty inches
of rain fell in one day. At Joyeuse, on the 9th of October, 1827,
thirty-one inches of rain fell in twenty-two hours. Previous to the
great floods of Moray, in 1829, the rain is described as being so thick
that the very air itself seemed to be descending in one mass of water
upon the earth. Nothing could withstand it. The best finished windows
were ineffectual against it, and every room exposed to the north-east was
deluged. The smaller animals, the birds, and especially game, of all
kinds, were destroyed in great numbers by the rain alone, and the mother
partridge, with her brood and her mate, were found chilled to death
amidst the drenching wet. It was also noticed, that, as soon as the
flood touched the foundation of a dry stone wall, the sods on the top of
it became as it were alive with mice, all forcing their way out to escape
from the inundation which threatened their citadel; and in the stables,
where the water was three feet deep, rats and moles were swimming about
among the buildings.
Public-domain text, read in full here on John Shaqi.
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