As the airflow encounters the mountain range, it is forced to rise; this is referred to as Orographic Lift. As the air mass gains altitude it quickly cools down adiabatically, which can raise the relative humidity to 100% and create Orographic clouds (clouds that develop in response to the forced lifting of air by the earth's topography).
- The type of clouds which will be formed depend on the type of air mass:
- Stable (layer type of clouds will form - STRATIFORM) - great horizontal extension, little vertical development: ST, SC,AS,NS,CI,CS.
- Unstable (heap type of clouds - CUMULIFORM) - extensive vertical extension: CU,TCU,CB,AC,CC.
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