Ch. 18 Sect. 1 & 3

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Created by:

mritkes  on November 3, 2011

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Earth Science

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Ch. 18 Sect. 1 & 3

water vapor
the most important gas for understanding atmospheric processes
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water vapor the most important gas for understanding atmospheric processes
precipitation rain, sleet, snow, and hail
water can change from one state of matter to another at the temperatures and pressures experienced at Earth's surface
sublimation the conversion of a solid directly to a gas
deposition the process by which water vapor changes directly to a solid
condensation change of state from a gas to a liquid
evaporation the process of converting a liquid to a gas
latent heat energy that is stored or released during a change of state of water
saturated air air that has reached its water vapor capacity
warm, saturated air contains more water vapor than cold air
relative humidity the ratio of air's water vapor content to its capacity to hold water vapor at the same temperature
relative humidity indicates how near the air is to saturation
dew point refers to the temperature to which air would have to be cooled to reach saturation
air has a high relative humidity when two temperatures read nearly the same on a psychrometer (no evaporation on the wet bulb)
increase in relative humidity when the water vapor content of air stays the same and the air temperature is lowered
smog NOT produced by condensation
dust and salt particles examples of condensation nuclei
stratus cloud type that is best described as sheets/layers that cover much or all of the lower sky
cumulus cloud type that consists of cloud masses with a cauliflower shape (puffy)
alto term used to describe clouds of middle height
nimbostratus cloud a low cloud that blankets the sky and often generates precipitation
cirrus cloud type that is in the high height range and wispy/feathery in shape/form
nimbus term that "rainy cloud"
cumulonimbus clouds often associated with thunder, lightning, and hail

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