The highly variable temperature rate at which still air changes with increasing altitude is referred to as the

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The highly variable temperature rate at which still air changes with increasing altitude is referred to as the environmental lapse rate. The moist adiabatic rate and dry adiabatic rate refer to the rate at which air cools as it rises and expands, and the lifting condensation level refers to the level at which air becomes saturated and begins to condense. While all of these factors are related to temperature changes with altitude, only the environmental lapse rate specifically refers to the highly variable rate of temperature change in still air.

The Highly Variable Temperature Rate at Which Still Air Changes