The temperature at which the air is saturated with water vapor.

The temperature at which the air is saturated with water vapor is essentially the dew point.

The dew point is the temperature of the gas at which the water vapor contained in the isobarically cooled gas becomes saturated above the flat surface of the water.

That is, it is the temperature of the air when the vapor in the air reaches saturation and begins to condense.

When the air is saturated with water, it begins to condense into water droplets – because the relative humidity reaches 100%.



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