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24-1 Air Masses
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Air Masses Hot air rises Cold air sinks
Low pressure Cold air sinks High pressure Differences in pressure causes wind
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How Air Moves From poles towards equator 3 wind belts in north
3 wind belts in south
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Coriolis effect – winds are deflected by Earth’s rotation
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Formation of Air Masses
Air mass – large body of air in which temperature and humidity are similar Stationary or slow
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Form in: Polar – cold and dry Tropical ocean – warm and moist
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Types of Air Masses Classified by source region
Temperature and humidity Ocean – maritime Land - continental
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Continental Form over large land masses Humidity low, dry
Stay in location for days or weeks
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cT – continental tropical
cP – continental polar Cold and dry cT – continental tropical Warm and dry
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Maritime Form over large bodies of water Higher humidity
Bring rain or fog
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mP – maritime polar mT – maritime tropical Moist and cold
Moist and warm
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North America Air Masses
Continental Polar cP – cold and dry From polar regions in Canada Moves south-sotheast
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From polar Pacific, polar Atlantic
Maritime Polar mP – cold and moist From polar Pacific, polar Atlantic Moves southeast, southwest-south
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Moves north-northeast
Continental Tropical cT – warm and dry From US southwest Moves north-northeast
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From tropical Pacific, tropical Atlantic
Maritime Tropical mT – warm and moist From tropical Pacific, tropical Atlantic Moves northeast, north-northwest
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