Chapter 5 - Atmospheric Moisture
Lapse Rates • Dry adiabatic lapse rate (DALR) –Rate at which rising parcel of unsaturated air cools. (1.0°C/100 m) • Saturated adiabatic lapse rate (SALR) - Rate at which rising parcel of saturated air cools. (0.5°C/100 m) • Dew point lapse rate – Rate at which dew point decreases with height. (0.2°C/100 m)
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