Curiosities of Science, Past and Present: A Book for Old and YoungTimbs, John
Science
Curiosities of Science, Past and Present: A Book for Old and Young
Timbs, John
Science
Thus the South Seas should supply mainly the water for the engine just
described, while the northern hemisphere condenses it; we should,
therefore, have more rain in the northern hemisphere. The rivers tell
us that we have, at least on the land; for the great water-courses of
the globe, and half the fresh water in the world, are found on the
north side of the equator. This fact is strongly corroborative of this
hypothesis. To evaporate water enough annually from the ocean to cover
the earth, on the average, five feet deep with rain; to transport it
from one zone to another; and to precipitate it in the right places at
suitable times and in the proportions due,--is one of the offices of
the grand atmospherical machine. This water is evaporated principally
from the torrid zone. Supposing it all to come thence, we shall have
encircling the earth a belt of ocean 3000 miles in breadth, from which
this atmosphere evaporates a layer of water annually sixteen feet in
depth. And to hoist up as high as the clouds, and lower down again,
all the water, in a lake sixteen feet deep and 3000 miles broad and
24,000 long, is the yearly business of this invisible machinery. What a
powerful engine is the atmosphere! and how nicely adjusted must be all
the cogs and wheels and springs and _compensations_ of this exquisite
piece of machinery, that it never wears out nor breaks down, nor fails
to do its work at the right time and in the right way!--_Maury._
THE PHILOSOPHY OF RAIN.
To understand the philosophy of this beautiful and often sublime
phenomenon, a few facts derived from observation and a long train of
experiments must be remembered.
1. Were the atmosphere every where at all times at a uniform
temperature, we should never have rain, or hail, or snow. The water
absorbed by it in evaporation from the sea and the earth’s surface
would descend in an imperceptible vapour, or cease to be absorbed
by the air when it was once fully saturated.
2. The absorbing power of the atmosphere, and consequently its
capability to retain humidity, is proportionally greater in warm
than in cold air.
3. The air near the surface of the earth is warmer than it is in
the region of the clouds. The higher we ascend from the earth, the
colder do we find the atmosphere. Hence the perpetual snow on very
high mountains in the hottest climate.
Now when, from continued evaporation, the air is highly saturated
with vapour, though it be invisible and the sky cloudless, if its
temperature is suddenly reduced by cold currents descending from
above or rushing from a higher to a lower latitude, its capacity to
retain moisture is diminished, clouds are formed, and the result is
rain. Air condenses as it cools, and, like a sponge filled with water
and compressed, pours out the water which its diminished capacity
cannot hold. What but Omniscience could have devised such an admirable
arrangement for watering the earth?
INORDINATE RAINY CLIMATE.
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