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 |
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。
出典 小学館デジタル大辞泉について 情報 | 凡例 |
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