Meteorology: The Science of the Atmosphere — John Shaqi
Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
The use of the aeroplane for making meteorological observations is
still quite limited, but will inevitably increase. One other device
gives promise of yielding valuable aerological information, on account
of its ability to rise to extraordinary altitudes. This is a special
form of rocket, recently invented by Prof. R. H. Goddard, which is
propelled by several successive discharges of an explosive in the
course of its upward flight, and with which the inventor thinks it will
be possible to explore the whole vertical extent of the atmosphere.
Meteorological apparatus for use with the Goddard rocket has been
planned by Mr. S. P. Fergusson of the Weather Bureau.
The atmosphere presses down upon the earth with a weight that, at sea
level, amounts to about 14.7 pounds to the square inch, on an average.
This pressure is, at any point, exerted equally in all directions; it
acts, for example, on the whole surface of the human body, and this
means that a man of average size lives under a burden of some seventeen
tons of air. He is not incommoded because the pressure from without is
balanced by that of the air that permeates his body.
The pressure of the atmosphere decreases upward at nearly the same
rate as its density. Thus on mountains and plateaus it is considerably
less than in lowlands. At no place is the pressure invariable, nor
is there a constant relation between pressure and altitude, but,
knowing approximately the average atmospheric pressure over the
earth’s surface, and knowing also the area of the latter, we can
compute in round numbers the total weight of the atmosphere--about
5,000,000,000,000,000 tons. This is about 1/1,200,000 of the entire
weight of the earth.
CHAPTER II
THE RESOURCES OF THE ATMOSPHERE
In the economic stress of our times much is heard about “natural
resources.” This phrase suggests to most people’s minds the store of
minerals, fuels, and oil locked up in the ground; the waters available
for drinking, washing, irrigation, power production, and navigation;
the forests and other natural growths of useful vegetation; and the
soil in which we raise our crops. A moment’s reflection, however,
will show that this is a one-sided enumeration. The resources of the
_atmosphere_ are as essential to humanity as those of the land and the
waters, if not more so.
Public-domain text, read in full here on John Shaqi.
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