As air descends in orographic rain,it warms initially at the dry adiabatic lapse rate.

Name: As air descends in orographic rain,it warms initially at the dry adiabatic lapse rate.
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As air descends in orographic rain, it warms at the dry adiabatic lapse rate, but this process occurs after the air has ascended, cooled, and condensed to form precipitation on the windward side of a mountain. The initial ascent leads to cooling and condensation, not warming.

As Air Descends in Orographic Rain,it Warms Initially at the Dry