Final answer:
The leeward side of a mountain generally receives less precipitation.
Step-by-step explanation:
The leeward (downwind) side of a mountain generally receives less precipitation. When moist air approaches a mountain range, it is forced to rise over the mountains. As the air rises, it cools and condenses, causing precipitation to occur on the windward (upwind) side. As the air descends on the leeward side, it warms and dries out, resulting in less precipitation on this side of the mountain.
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