The new air world : $b The science of meteorology simplifiedMoore, Willis L. (Willis Luther)
Science
The new air world : $b The science of meteorology simplified
Moore, Willis L. (Willis Luther)
Meteorology
Even more calamitous would be the floods of springtime, for melting
snows and falling rains would spread over and erode the cultivated
fields of the husbandman instead of being carried away by the open
channels of streams, as is largely done now.
=The Freezing of Fresh and of Salt Bodies of Water.= The freezing of
water does not take place upon the surface of water only, as many
suppose. Congelation takes place about millions of minute atoms of
matter carried by the water in suspension. Water expands in the
process of freezing and each particle of ice, no matter in what part
of the body of water it is formed, immediately rises to the surface
because of the gain in its buoyance as it changes from the liquid to
the solid form.
When the surface of water cools by radiation to a cooler air it
gains in specific gravity and sinks and warmer water comes up to
take its place and in turn be cooled and sink; thus a circulation is
established which continues in fresh water until every part of the
body of water has fallen to 39° and in salt water to 28°. At these
temperatures the two waters reach their maximum density. With the
further cooling of salt water particles of ice form and rise to the
top, as already described. With the cooling of fresh water below 39°
the law that holds good for all higher temperatures is reversed and
expansion of volume begins, which continues until 32° is reached.
Therefore, fresh water of any temperature between 39° and 32° may
float upon water that is considerably warmer; in fact, it has less
specific gravity at 32° than at 46°. At 32° that which was a liquid
becomes a solid and still further suddenly expands its volume.
=The Cold of Ocean Bottoms.= Few have any idea of the enormous volume
of cold water that lies upon the surface of the earth, three fourths
of which is covered with oceans whose depths average two miles and
in many places are five miles. Below one mile in depth these oceans
are always at about the freezing point of salt water, which is 28°,
except in the tropics, where it is but little warmer, varying between
34° and 36°.
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