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

A)Adiabatic cooling due to uplift
B)Latent heat release during condensation
C)Orographic lift forcing air upwards
D)Increased surface friction slowing wind

💡 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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