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
rises and passes along the ceiling to the colder parts of the room,
gradually parting with its heat until it is no warmer than the air
next adjacent to it, and slowly settling to the floor as the cold
air beneath it moves toward the stove, is warmed and sent aloft,
the first air finally making a complete circuit and returning to
the stove again. In this way the heat is distributed by convection
throughout the whole room. When one part of the earth’s surface
becomes hotter than another a similar action takes place on a large
scale. The region of greater temperature warms the air above it, and
the surrounding denser air flows in along the surface, forcing the
lighter air to rise, when it in turn is similarly warmed and driven
up.
The clear waters of lakes and rivers and of the ocean permit the
passage of heat waves to a considerable depth before they are
completely absorbed. On a cold day in winter, when the sun is shining
brightly, a room with spacious windows may become as warm as though
heated by a furnace, simply by the capacity of the glass in the
windows to transmit the heat waves of the sun without considerable
absorption, and at the same time prevent the escape of the longer
heat waves that are radiated from the interior walls of the room.
This capacity of matter to transmit heat waves without absorption
is called diathermancy. The clear atmosphere is an exceedingly good
transmitter, and rock salt is one of the best of all solids.
The capacity of a body to transmit light without absorbing it and
becoming luminous is called transparency. Air freed of dust motes
is almost perfectly transparent. In this state it is said to be
optically pure. But the ordinary air of nature, with its moisture
and dust, absorbs most of the blue wave lengths and also many of the
longer ones of the other colors of the spectrum.
The capacity of a body for heat is called its specific heat. With
but few exceptions the specific heats of liquids are much greater
than those of solids or gases. It requires ten times the quantity of
heat to raise a pound of water one degree that it does a pound of
iron. Ice has the greatest specific heat of any of the solids, except
paraffin and wood.
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