Ascending fog - Kasshogiri

Japanese: 滑昇霧 - かっしょうぎり
Ascending fog - Kasshogiri
Fog formed when air blowing up the slope of a mountain cools due to adiabatic expansion. Rising fog.

Source: About Shogakukan Digital Daijisen Information | Legend

Japanese:
山の斜面を吹き上げる空気が断熱膨張によって冷却してできる霧。上昇霧。

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