Which mechanism explains how mountain ranges enhance precipitation in the windward slopes, creating rain shadow effects?

💡 Explanation

When moist air encounters a mountain range, orographic lift forces the air mass to rise, causing it to cool and condense, resulting in enhanced precipitation on the windward side, and a rain shadow on the leeward side. Therefore orographic lift explains that precipitation pattern, rather than adiabatic cooling, which occurs in stable atmospheric conditions.

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