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The rain shadow effect explains why Vail may have a higher precipitation average than Monte Vista.
The precipitation average in Vail could be higher than in Monte Vista due to the rain shadow effect. When winds carry moist air up a mountain range, the air cools, condenses, and causes precipitation on the windward side, resulting in less precipitation on the leeward side, creating a dry region known as a rain shadow. This phenomenon leads to varying precipitation levels on different sides of the mountain range.
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