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Chapter 14 Section 3 Air Movement & Wind
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Wind: the movement of air caused by differences in air pressure.
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Coriolis effect: the curving of the path of a moving object from an otherwise straight path due to Earth’s rotation.
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Differences in air pressure causes wind.
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Warm air rises at the equator & cold air sinks at the poles causes differences in air pressure around Earth.
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Air moves in patterns of high & low pressure that are part of convection cells.
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In the Northern Hemisphere, winds traveling north curve to the east because of the Coriolis effect.
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Global winds that blow from west to east are called westerlies.
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Global winds that blow almost to the equator from 30 degree latitude are called trade winds.
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A wind belt that carries cold arctic air over the United States is called a(n) polar easterly.
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Local winds are affected by local geographic features.
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Mountains & valley breezes are caused by differences in temperature & elevation.
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