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
=Influence of Lakes and Rivers.= With the exception of contributing
to the formation of occasional fogs over their surfaces and the
adjacent low lands, through the rising of warm water vapor into
the cold air that often collects at the bottom of valleys during
nighttime, rivers exercise little influence on climate. Lakes exert
a modifying influence on the temperature of places near their shores
but only for a few miles therefrom, and they are too small to exert
any appreciable influence on rainfall. If one examine charts showing
the average rainfall for the United States by seasons, he will
observe that the amount gradually shades off as the distance from
the Gulf or Ocean increases, without any relation whatever to the
five Great Lakes. Deserts exist on either side of the Caspian Sea,
although it slightly increases the rain of the Elburz Mountains to
the south. If these great bodies of water do not influence the
rainfall, how ridiculous to assume that the changing of forest areas
to other forms of vegetation possibly can affect precipitation or
influence droughts. Stress is laid on the fact that some land is left
bare and then is eroded into deep gullies. This is true, but the
fault is one that may be corrected by a proper system of plowing and
cultivation. And at most the area so eroded is so infinitesimal in
comparison to the vast regions changed from forests to growing crops
as to be negligible.
[Illustration: CHART 14.—MEAN ANNUAL ISOTHERMS (Buchan).]
=Influence of Ocean Currents on Climate.= Climates are markedly
influenced by the currents of oceans. Charts 15 and 16 show the
normal wind circulations of the globe; note that the centers of the
great swirls are coincident with the location of the High and the
Low centers of action located on Charts 1 and 2. Next observe Chart
13, showing the ocean currents, and it will be seen at once how
closely the circulation of the great ocean currents follows that of
the winds, due to the friction of the air upon the water, and to
the interposition of bodies of land that turn about or deflect the
currents.
[Illustration: CHART 15.—NORMAL WIND DIRECTION AND VELOCITY FOR
JANUARY AND FEBRUARY (Köppen).]
[Illustration: CHART 16.—NORMAL WIND DIRECTION AND VELOCITY FOR JULY
AND AUGUST (Köppen).]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account