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Published byAlice Dean Modified over 9 years ago
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Winds that blow steadily from specific directions over long distances
Global winds Winds that blow steadily from specific directions over long distances
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Created by unequal heating of earth’s surface
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Example of sun’s rays with a flashlight
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Global convection currents
Movement of air between the equator and the poles produce global winds
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Coriolis effect makes winds curve
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Prevailing Westerlies
Main Global wind belts Prevailing Westerlies Trade Winds Polar Easterlies
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Trade winds Blow from the horse latitudes (30oN & S) toward the equator Sailors relied on trade winds to carry cargoes from Europe to the West Indies and South America
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Prevailing Westerlies
Blow from the west to the east (name comes from where winds blow FROM) Play an important part in the weather of the United States
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Polar easterlies Cold air from the poles sinks and flows back toward lower latitudes The Coriolis Effect shifts these winds to the west, so they are called EASTERLIES. Has a major effect on the weather of the United States
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Regions near the equator with little or no wind where warm air rises
Doldrums Regions near the equator with little or no wind where warm air rises
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Horse latitudes Calm areas of falling air 30* N & S Called horse latitudes because sailors ran out of food and water for their horses here and had to throw them overboard
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Jet Streams About 10 km above Earth’s surface Blow from west to east at km/h Planes flying east can save time and fuel by flying in the jet stream
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