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Atmospheric Circulation and Weather Systems
The characteristics are:
i. It deflects the wind to the right direction in the northern hemisphere and to the left in the southern hemisphere. The deflection is more when the wind velocity is high.
ii. The Coriolis force is directly proportional to the angle of latitude.
iii. It is maximum at the poles and is absent at the equator.
Sponsor Area
Sponsor Area
Sponsor Area