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Atmospheric Pressure
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gradients result from differential heating
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Coriolis Effect
Coriolis
Effect is the apparent deflection of motion of any object traveling over the spinning
Earth. A famous example is Long Max, a giant railway cannon that kept missing its
target (although hugely exaggerated below). During several minutes of elapsed time
while the shell was airborne, the target had moved east of its original position at the
time the shell was fired. This same type of deflection also affects air molecules in
wind.
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The
reason Coriolis Effect occurs is because the Earth spins, at a rate of 15� of longitude
per hour ("angular velocity"). However, because longitude converges at the
Poles, the DISTANCE velocity is greater at lower latitudes than at higher latitudes.
Furthermore,
the direction of deflection differs between latitudinal hemispheres. Going FROM
their original positions, objects deflect clockwise in the northern hemisphere and
counterclockwise in the southern hemisphere.

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Because
of Coriolis Effect, aircraft pilots do not aim their planes at the intended destination
when they take off! Instead, they aim for where the destination WILL be after the
elapsed flight time. Assuming the plane retains the eastward momentum of its takeoff
location, the pilot must add or reduce distance and alter compass direction to compensate
for the expected time flying over the moving Earth.

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Yours
is visit # to this Web page since 10MAY97.
N. C. Heywood maintains this page, last updated
20JUL99. |