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
As the result of the explorations of the atmosphere made by the
institution at Mount Weather there was ready for our fighting air men
at the front, immediately on our entry into the World War, a fund of
useful information concerning a region that but a short time before
was entirely uncharted. The instruments carried by the exploring
kites and balloons had keen scientific eyes and they recorded on
clock-timed cylinders what they saw. Thus did the air pilot know
much about the direction and the force of the wind that he would
encounter as he rose, the altitude where he would pass above clouds,
the degree of cold that he would encounter, etc. He was told that the
temperature would fall about one degree for each three hundred feet
of his ascent until he reached the top of the storm stratum at six
or seven miles, and that if he could reach that altitude he would
observe a most wonderful phenomenon: the temperature no longer would
fall with gain in altitude; he would enter a cold but an equally
heated stratum, without finding any temperatures lower than were
encountered upon entering the region, which is always about seventy
degrees below zero.
If the aërial explorer could stop his ship and keep it at an altitude
of about one and one half miles for twenty-four hours he would be
startled to find that the coolest time of the period was during the
daytime, not during the night, as he had expected to find it.
In the future the traveler in the upper reaches of the atmosphere
will carry oxygen and make the kind of air that he wishes to breathe,
and he will properly protect himself against the cold of his new
world, which he will find deficient in dust motes and doubtless
entirely wanting in the bacteria of putrefaction and of disease.
There will be no clouds to obscure his vision; no rain or snow. He
will not often ascend above the region where there are not some dust
motes to scatter and diffuse a part of the solar rays and give him at
least a partial illumination.
Public-domain text, read in full here on John Shaqi.
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