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Published bySuzan Gibson Modified over 8 years ago
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Air Masses and Fronts
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Air Mass A large body of air A large body of air At least 1,000 miles across At least 1,000 miles across Uniform temperature and humidity Uniform temperature and humidity Flows as one unit Flows as one unit
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Air Mass Four main types Four main types –Cold (polar) –Warm (tropical) –Water (maritime) –Land (continental) Combinations Combinations –Maritime tropical –Maritime polar –continental tropical –Continental polar
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Fronts When two air masses meet When two air masses meet
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Fronts Warm front—When a warm air mass overrides a cold area, it rises slowly, creating nimbostratus, altostratus or cirrostratus clouds. This can produce light precipitation. Warm front—When a warm air mass overrides a cold area, it rises slowly, creating nimbostratus, altostratus or cirrostratus clouds. This can produce light precipitation.
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Fronts Cold front—When a cold air mass overrides a warm area, it pushes the warm air up forcefully, creating cumulus and cumulonimbus clouds. Cold fronts often produce thunderstorms and very bad weather. Cold front—When a cold air mass overrides a warm area, it pushes the warm air up forcefully, creating cumulus and cumulonimbus clouds. Cold fronts often produce thunderstorms and very bad weather.
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Fronts Stationary front— When a cold air mass and warm air mass flow side-by-side, and neither mass invades the other, weather can by unpredictable. It most often resembles a warm front, with light rain if any precipitation occurs. Stationary front— When a cold air mass and warm air mass flow side-by-side, and neither mass invades the other, weather can by unpredictable. It most often resembles a warm front, with light rain if any precipitation occurs.
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Fronts Occluded front— When two cold air masses trap a warm air mass, they push the warm air up. The boundary that exists is between two similar air masses: cold and cooler air. Clouds and precipitation are likely. Occluded front— When two cold air masses trap a warm air mass, they push the warm air up. The boundary that exists is between two similar air masses: cold and cooler air. Clouds and precipitation are likely.
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Mid-latitude Cyclones Severe storms that develop between tropical and polar air masses in mid- latitude regions around low-pressure centers. Severe storms that develop between tropical and polar air masses in mid- latitude regions around low-pressure centers.
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