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Cloud Formation
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Air Pressure Caused by the weight of the air above it
Decreases with elevation Barometric pressure Barometer Millibars / mm Hg
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Pressure and Temperature
When pressure drops air expands and cools
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Cloud Formation Air rises Air expands Dew point is reached
decrease in pressure Air expands Temperature decreases Dew point is reached Water vapor condenses on tiny particles (condensation nuclei)
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Processes That Lift Air
Mountains
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windward leeward
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Processes That Lift Air
Fronts Boundary between two different air masses Warm air is forced up by more dense cold air
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Source region – area where air masses originate
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Processes That Lift Air
Convergence
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