The General Circulation of the Atmosphere. Weather with different scales. What we need to know for today. Pressure gradient force: from H igh to L ow pressure Coriolis force (effect): Results from the rotation of the planet. Maximum at the poles and no effect at the equator.
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in the tropics.
sinking air that creates high surface
pressure in the polar region.
the surface winds from the poles towards
from the equator towards the poles.
Observing global winds