The moist adiabatic rate varies as a function of both temperature and moisture content.

Name: The moist adiabatic rate varies as a function of both temperature and moisture content.
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The moist adiabatic rate is the rate at which a parcel of moist air cools as it rises. It varies with temperature and moisture content because as the parcel rises, the temperature decreases and moisture may condense, releasing latent heat and affecting the rate of cooling.

The Moist Adiabatic Rate Varies as a Function of Both