Adiabatic Lapse Rate
Adiabatic Lapse Rate :
The rate at which ascending air cools and descending air warms, given that no heat is added or taken away. The rate for dry air (DALR) is based on 5.4 F per 1000' altitude (1 per 100 meters). Moist or saturated rates (SALR) vary with barometric pressures and temperatures and must be adjusted for accuracy
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