Final answer:
Orographic lift causes more rain on the windward mountain side than the leeward side due to the process of condensation and precipitation.
Explanation:
More rain falls on the windward side of a mountain than on the leeward side due to orographic lift. When moist air from the ocean hits the mountain, it is forced to rise, cool, and condense, leading to precipitation on the windward side. The leeward side, on the other hand, experiences dry air descending, warming, and inhibiting precipitation, creating a 'rain shadow' effect.
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