DEW

Adair's New Encyclopedia · 1923 · p. 7
small drops of water deposited during the night on substances which po e good radiating powers and which consequently cool quickly below the temperature of the surrounding air. As a result, the air which is in direct contact with such a substance becomes cooled until the dew point is reached, that temperature at which the water vapor already in the atmosphere is the maximum quantity the air can hold.
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