A History of Science — Volume 3Williams, Henry Smith
History
A History of Science — Volume 3
Williams, Henry Smith
Science -- History
"According to the theory, nothing is required for the production of rain
besides the mixture of portions of the atmosphere with humidity, and of
mixing the parts that are in different degrees of heat. But we have seen
the causes of saturating every portion of the atmosphere with humidity
and of mixing the parts which are in different degrees of heat.
Consequently, over all the surface of the globe there should happen
occasionally rain and evaporation, more or less; and also, in every
place, those vicissitudes should be observed to take place with some
tendency to regularity, which, however, may be so disturbed as to be
hardly distinguishable upon many occasions. Variable winds and variable
rains should be found in proportion as each place is situated in an
irregular mixture of land and water; whereas regular winds should be
found in proportion to the uniformity of the surface; and regular rains
in proportion to the regular changes of those winds by which the mixture
of the atmosphere necessary to the rain may be produced. But as it will
be acknowledged that this is the case in almost all this earth where
rain appears according to the conditions here specified, the theory is
found to be thus in conformity with nature, and natural appearances are
thus explained by the theory."(1)
The next ambitious attempt to explain the phenomena of aqueous meteors
was made by Luke Howard, in his remarkable paper on clouds, published in
the Philosophical Magazine in 1803--the paper in which the names cirrus,
cumulus, stratus, etc., afterwards so universally adopted, were first
proposed. In this paper Howard acknowledges his indebtedness to Dalton
for the theory of evaporation; yet he still clings to the idea that
the vapor, though independent of the air, is combined with particles of
caloric. He holds that clouds are composed of vapor that has previously
risen from the earth, combating the opinions of those who believe
that they are formed by the union of hydrogen and oxygen existing
independently in the air; though he agrees with these theorists that
electricity has entered largely into the modus operandi of cloud
formation. He opposes the opinion of Deluc and De Saussure that clouds
are composed of particles of water in the form of hollow vesicles
(miniature balloons, in short, perhaps filled with hydrogen), which
untenable opinion was a revival of the theory as to the formation of all
vapor which Dr. Halley had advocated early in the eighteenth century.
Public-domain text, read in full here on John Shaqi.
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