Air Stability
Adiabatic Processes No heat is added / removed from the moving air parcel by the external environment because of fast movement of the air parcel. All temperature changes within the air parcel are due to expansion / contraction.
1000m ground
Warm air Cooler than surrounding cloud Condensation level Stable air Unstable air precipitation Energy loss Air stops rising
Causes of Cooling
Orographic Cooling
Rising air
Frontal Cooling
Front Condensation Rising air
Thermal Cooling
Rising air
Precipitation
Prepared by Humanities Unit Curriculum Development Institute Education Department