Amount of water vapour in 2nd phase of atmosphere of earth was-
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The amount of water in the air is variable. It can go from zero to a maximum: the saturation pressure, which is a function of temperature:
Relative humidity is the actual vapor pressure divided by the saturation pressure at the current air temperature. The dew point is the temperature to which the air would have to drop for the saturation vapor pressure to equal the actual pressure, at which point water would condense. Dew point is actually a better indicator of the absolute concentration of water vapor in air than relative humidity, because it is independent of temperature.
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The amount of water in the air is variable. It can go from zero to a maximum: the saturation pressure, which is a function of temperature:
Explanation:
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