Refer to figure.
HILL/OROGRAPHIC FOG. Usually stratiform cloud (ST, SC) whose base is lower than the summit of the hills.
- Formed when humid stable air is forced to ascend along the side of a mountain or hill or by the normal turbulence action producing ST and SC.
- Formed during the day or night.
- As the air rises, it cools adiabatically => condensation level is reached, and a cloud is formed.
- Hill fog requires a wind up the slopes of a mountain and is promoted by high humidity. The hill fog quickly disappears if the wind changes.
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