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Global & Local Winds
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Wind Wind is created by differences in air pressure.
The greater the pressure the faster the wind moves. Equator: warmer less dense air rises and creates an area of high pressure. Poles: colder, more dense air sink & creates areas of high pressure. Air moves from high to low pressure (poles to the equator)
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How does the Sun’s energy produce wind?
The unequal heating of Earth by the sun causes differences in air pressure. This causes convection currents, which produce wind.
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Pressure Belts Equator: warm air rises & moves away & begins to cool,
at 30 degrees N & S latitude are high pressure belts. Poles: cold air sinks & moves away & begins to warm, creating a low pressure belt around 60 degrees N & S latitude. Convection Cells: circular patterns caused by the rising & sinking of air. Coriolis Effect: the curving of moving objects, such as wind, by the Earth’s rotation. N. Hem. curves right S. Hem curves left
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Two Types of Wind Local Winds: move short distances & can blow from any direction. Global Winds: are part of a pattern of air circulation that moves across the Earth (travel longer distances). Global winds include: trade winds, westerlies, & polar easterlies.
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More about the types of WIND!
Trade winds: blows from 30 degrees latitude to the equator. They meet in an area of low pressure around the equator called the doldrums (little wind b/c of warm rising air). About 30 degrees N and S. latitude, high pressure (horse latitudes) winds are weak.
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Westerlies & Easterlies
Westerlies: found between 30 degrees & 60 degrees latitude. They flow toward the poles in opposite direction of the trade winds. Polar Easterlies: cold, sinking air wind belts that extend from the poles to 60 degrees N & S latitude.
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Jet Streams Jet streams are narrow belts of high speed winds that blow in the upper troposphere and lower stratosphere. They help meteorologists (track storms) and pilots (save time & fuel). Local winds are influenced by the geography of an area. sea and land breezes and mountain and valley breezes.
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