The dew-point temperature refers to the temperature at which an air mass reaches saturation.

Name: The dew-point temperature refers to the temperature at which an air mass reaches saturation.
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The dew-point temperature is the temperature at which an air mass becomes saturated with water vapor, leading to the formation of dew or fog. It is the point at which the air cannot hold any more water vapor, and any further cooling of the air will result in the condensation of moisture.

The Dew-Point Temperature Refers to the Temperature at Which an Air