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any form of water that falls from a cloud |
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the process of changing a liquid to a gass |
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the opposite process where water vapor changes to the liquid stat |
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the conversion of a solid directly to a gas, without passing the liquid state |
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the conversion of a vapor directly to a solid |
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the general term for the amount of water vapor in the air |
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the number of vapor molecules returning to the survace will balance the number leaving |
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the temperature to which a parcel of air would need to be cooled to reach saturation |
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realative humidity is measure using this |
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rate of cooling or heating applies only to unsaturated air |
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slower rate of cooling caused by the addition of latent heat |
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elevated terrains, such as mountains act as barriers to air flow |
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when masses of warm and cold air collide |
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the most stable conditions when air temperature increases with height |
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serve as surfaces for water-vapor condensation |
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high white and thin clouds |
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clouds consisting of rounded individual cloud masses |
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best described as sheets or layers that cover much or all of the sky |
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a cloud with its base at or very near the ground |
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water in the liquid state below 0 degrees celcius |
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when air is saturated with respect to water |
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collision-coalescence process |
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in warm clouds, the mechanism that forms raindrops |
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