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Rapid movement Gradual movement
Types of Air Masses Rapid movement Gradual movement
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Gradual Movement Air mass- a huge section of the lower troposphere that has the same kind of weather throughout
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Air Masses Maritime tropical (mT) from the tropical seas, warm and humid
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Air Masses Continental tropical (cT) from the tropical land masses, hot and dry
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Air Masses Maritime polar (mP) from the cold ocean water, cold and humid
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Air Masses Continental polar (cP) from land in high latitudes, cold and dry
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Air Masses Continental Arctic (cA) from ice covered Arctic regions, very cold and dry
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Fronts Gradual movement Where one air mass is displacing another
The boundary between two air masses, most precipitation comes with fronts Warm Cold Stationary
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Warm Fronts Warm air pushing ahead and displacing cold air
Weather- slow moving, steady rain or snow
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Cold Front Cold air is advancing and taking over warm air
Weather- quick showers and thunderstorms, temperatures fall fast
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Stationary Front Neither front is being displaced, no movement
Weather- much like a warm front
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