Mountains often have rainy climates on their windward slopes and dry climates on their leeward slopes.

Name: Mountains often have rainy climates on their windward slopes and dry climates on their leeward slopes.
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This is because as moist air is pushed up over the mountain, it cools and the moisture condenses, leading to precipitation on the windward side. On the leeward side, the air has already lost most of its moisture, leading to dry conditions. This is known as the "rain shadow effect."

Mountains Often Have Rainy Climates on Their Windward Slopes and Dry