Global Winds: High, Convection Currents, Poles, Coriolis Effect, Low, Equator 1) The wind direction is affected by the (caused by the Earth's rotation) and (hot air rising, cold air sinking) in the atmosphere. 2) Air moves from pressure to pressure. 3) At the cold air sinks and moves along the surface of the earth towards the 4) Warm air rises at the and moves through the upper troposphere towards th 5) Air sinks at the 6) Air rises at the because it has pressure. because it has pressure.

BIOLOGY:CONCEPTS+APPL.(LOOSELEAF)
10th Edition
ISBN:9781305967359
Author:STARR
Publisher:STARR
Chapter43: The Biosphere
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Global Winds: High, Convection Currents, Poles, Coriolis Effect, Low, Equator
1) The wind direction is affected by the
(caused by the Earth's rotation) and
(hot air rising, cold air sinking) in the atmosphere.
2) Air moves from
pressure to
pressure.
3) At the
cold air sinks and moves along the surface of the earth towards the
4) Warm air rises at the
and moves through the upper troposphere towards the
5) Air sinks at the
6) Air rises at the
because it has
pressure.
because it has
pressure.
Transcribed Image Text:Global Winds: High, Convection Currents, Poles, Coriolis Effect, Low, Equator 1) The wind direction is affected by the (caused by the Earth's rotation) and (hot air rising, cold air sinking) in the atmosphere. 2) Air moves from pressure to pressure. 3) At the cold air sinks and moves along the surface of the earth towards the 4) Warm air rises at the and moves through the upper troposphere towards the 5) Air sinks at the 6) Air rises at the because it has pressure. because it has pressure.
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