Which mechanism creates the rain shadow effect on the leeward side of a mountain range?

💡 Explanation

When moist air is forced to rise over a mountain range, orographic lift occurs, causing adiabatic cooling, which condenses moisture and releases precipitation on the windward side. Therefore, the rain shadow effect results on the leeward side, rather than sea breezes, Coriolis-deflected winds or air mass convergence, as these mechanisms do not depend on a mountain range.

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