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Weather Water in the Atmosphere May 14, 2008
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Precipitation Precipitation is any form of water that falls from a cloud. Water vapor is the source of all condensation and precipitation. When it comes to understanding atmospheric processes, water vapor is the most important gas in the atmosphere.
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Changing State The process of changing state requires that energy is transferred in the form of heat. Latent heat is heat used to melt ice that does not produce a temperature change.
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Water’s Changes of State
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Humidity Humidity is the term for the amount of water vapor in the air. Saturation describes the state when the number of molecules evaporating equals the number of molecules condensing.
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Relative Humidity Relative Humidity is a ratio of the air’s actual water vapor content compared with the amount of water vapor air can hold at that temperature.
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Temperature and Relative Humidity When the water-vapor content of air remains constant, lowering air temperature causes an increase in relative humidity, and raising air temperature causes a decrease in relative humidity
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Dew Point Dew point is the temperature to which a parcel of air would need to be cooled to reach saturation.
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Assignment Read pg. 504-509 Complete 18-1 ws
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