Source: Treehugger.com

Rain shadow is a fascinating geographical phenomenon that occurs when a mountain range obstructs the path of prevailing winds, causing them to rise and cool. As the air ascends, it releases moisture in the form of rainfall or snow on the windward side of the mountains. However, once the air descends on the leeward side, it becomes dry and creates a rain shadow effect, leading to arid and desert-like conditions.

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