Light Science for Leisure Hours: A series of familiar essays on scientific subjects, natural phenomena, &c.Proctor, Richard A. (Richard Anthony)
Science
Light Science for Leisure Hours: A series of familiar essays on scientific subjects, natural phenomena, &c.
Proctor, Richard A. (Richard Anthony)
Science
The modern theories of the correlation of force suffice to show how
enormous a loss a country suffers when there is a failure in the
supply of rain, or when that supply comes out of its due season. When
we consider rain in connection with the causes to which it is due, we
begin to recognise the enormous amount of power of which the ordinary
rainfall of a country is the representative; and we can well understand
how it is that ‘the clouds drop fatness on the earth.’
The sun’s heat is, of course, the main agent—we may almost say the
only agent—in supplying the rainfall of a country. The process of
evaporation carried on over large portions of the ocean’s surface
is continually storing up enormous masses of water in the form of
invisible aqueous vapour, ready to be transformed into cloud, then
wafted for hundreds of miles across seas and continents, to be finally
precipitated over this or that country, according to the conditions
which determine the downfall of rain. These processes do not appear, at
first sight, indicative of any very great expenditure of force, yet in
reality the force-equivalent of the rain-supply of England alone for a
single year is something positively startling. It has been calculated
that the amount of heat required to evaporate a quantity of water which
would cover an area of 100 square miles to a depth of one inch would
be equal to the heat which would be produced by the combustion of half
a million tons of coals. The amount of force of which this consumption
of heat would be the equivalent corresponds to that which would be
required to raise a weight of upwards of one thousand millions of tons
to a height of one mile. Now, when we remember that the area of Great
Britain and Ireland is about 120,000 square miles, and that the annual
rainfall averages about 25 inches, we see that the force-equivalent
of the rainfall is enormous. All the coal which could be raised from
our English coal mines in hundreds of years would not give out heat
enough to produce England’s rain-supply for a single year. When to this
consideration we add the circumstance that the force of rain produces
bad as well as good effects—the former when the rain falls at undue
seasons or in an irregular manner, the latter only when the rainfall
is distributed in the usual manner among the seasons—we see that an
important loss accrues to a country in such exceptional years as the
present.
Public-domain text, read in full here on John Shaqi.
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