The amount of water vapor in the air is referred to as humidity, which can be measured and expressed in several ways. Absolute humidity is a direct measure of the amount of water vapor in a given volume of air, specific humidity is the mass of water vapor in a given mass of air, and relative humidity is the amount of water vapor in the air compared with the amount that could be there if the air
were saturated. The dew point is the temperature at which the air becomes saturated.
a. example
b. explanation c. definition
c
Language Arts & World Languages
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