Aërial Navigation: A Popular Treatise on the Growth of Air Craft and on Aëronautical MeteorologyZahm, Albert Francis
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Aërial Navigation: A Popular Treatise on the Growth of Air Craft and on Aëronautical Meteorology
Zahm, Albert Francis
Aeronautics; Meteorology
In like manner the mountain-and-valley winds may be used by the
skillful aëronaut. It is well known that these flow up the courses of
rivers, cañons and land slopes generally by day, but at night reverse
their course and pour down again with considerable force. For this
reason experienced hunters place their camp fires below tent in a
sloping valley. The strength of the breeze depends, of course, upon
the daily range of temperature, and the steepness and expanse of the
slope. Such winds are deftly used by the masters of soaring flight, the
great robber and scavenger birds, and no doubt may be used by men in
motorless aëroplanes, to gain elevation, and journey great distances
without expenditure of energy.
CHAPTER XVI
CYCLONES, TORNADOES, WATERSPOUTS
Besides the periodic winds so far treated, there are prominent aërial
movements having no regular course or season. These are the nonperiodic
winds which so exercise or perplex the weather forecaster and those who
confide in him. In general such winds are of a temporary character,
arising from an unstable condition of the air in some locality, or
from unequal heating, either of which causes may generate, or briefly
sustain, an updraught, with its attendant gyration. Owing to the
whirling character of such ascending currents, they have received
various significant names, such as cyclone, tornado, whirlwind; the
three terms applying to vortices in decreasing order of magnitude. Each
in turn may be treated briefly.
The cyclone is a temporary large gyratory wind. It may last a few hours
or a few days. It may measure fifty to a hundred miles across, or it
may measure more than a thousand miles. On the weather map it is in
general marked by a group of closed isobars, showing a considerable
pressure gradient toward a small internal area where the pressure is
a minimum. To an observer looking about the earth’s surface and lower
levels of the atmosphere, the cyclone appears merely as an ordinary
wind, accompanied perhaps by rain or snow. It is not a swiftly rotating
narrow column, or cone of air, like a tornado or whirlwind, full of
gyrating dust and débris.
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