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The Atlantic Monthly, Volume 01, No. 3, January, 1858 by Various
page 46 of 293 (15%)
A storm not only disturbs the lower winds, but its influences reach
even to the upper movements. The sudden expansion and rising of the
rainy air delay these movements, which afterwards react as violent
winds.

The forces stored away by the gradual rise of vapor and its
absorption of heat, and then suddenly exhibited in a mechanical form
by the effects of rain, afford an illustration of that principle of
conservation and economy of power, of which there are so many
examples in modern science. No power is ever destroyed. Whether
exhibited as heat or mechanical force, in the products and forces of
chemical or of vital action, in movement or in altered conditions of
motion,--whether changed by the growth of plants into fuel or into
food, and converted again to heat by combustion or by vital processes,
and brought out as mechanical power in the steam-engine or in the
horse,--it is still the same power, and is measured in each of its
forms by an invariable standard. It first appears as the heat of the
sun, and a portion escapes at once back into space, while the rest
passes first through a series of transformations. A part is changed
into moving winds or into suspended vapor, and a part into fuel or
food. From conditions of motion it is changed into motion; from
motion it is changed by friction or resistance into heat, electric
force, molecular vibrations, or into new conditions of motion, and
passing through its course of changes, it remains embroiled in its
permanent effects or escapes into space as heat.

Though mechanical science will probably never be able to predict the
beginning or duration of storms, it will yet, doubtless, be able to
account for all their general features, and for such distinct local
peculiarities as observation may determine. Great advancement has
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