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
Figure 14 gives an illustration of what would be the movement of
air inward to a cyclone on a non-rotating earth. The winds would
blow along radial lines for a time, but, converging together as they
began to ascend, they doubtless would soon set up a gyration about
the center. On a non-rotating earth this gyration would be clockwise
as often as it would be anti-clockwise, but on a rotating earth the
gyration can be in but one direction. (Figure 15.) Even tornadoes,
whose diameters of rotation are never but a few hundred feet, obey
this law. In little dust whirls, in which the movements of air may
be comprehended from the motion of the trash that is whirled about
and which are tornadoes in miniature, the direction of gyration may
be either way. They are too small for the deflecting force to be
appreciable, and it may be that the tornado is forced to take its
direction of gyration from the cyclone in whose southeast quarter it
has its origin.
[Illustration: FIG. 15.—Deflection of wind due to earth’s rotation.]
=How Wind Velocity Increases with Altitude.= Figure 16 shows how
the velocity of the wind increases with elevation in the free air
up to five thousand meters (about three miles). The average for the
year, for the summer and for the winter, is given. It increases most
rapidly up to six hundred meters in summer and up to eight hundred
meters in winter. From these two heights there is a steady and
pronounced slowing down of the wind up to one thousand meters; after
which it increases up to five thousand meters, and how far beyond we
know not. In winter there is a singular acceleration of velocity in
the stratum between two thousand and twenty-five hundred meters and
then no increase for the next five hundred meters; after which there
is a uniform and steady gain up to five thousand meters. Starting at
two hundred and seventy meters, the average velocity for the year is
3½ meters per second, or about 7¼ miles per hour. At five thousand
meters altitude the average for the year is 11¼ meters per second, or
about 27 miles per hour.
[Illustration: FIG. 16.—Annual, summer, and winter wind velocities,
with altitude. 1, 1850 feet; 2, 2467 feet; 3, 3083 feet; 4, 15,417
feet.]
CHAPTER IX
HOW TO FORECAST FROM THE DAILY WEATHER MAP
IT IS NOT DIFFICULT TO BECOME WEATHERWISE AND THEREBY TO GAIN
ADVANTAGES IN HEALTH, HAPPINESS, AND BUSINESS
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