Rain shadows develop on the leeward side of topographic barriers.

Name: Rain shadows develop on the leeward side of topographic barriers.
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Question

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This is a correct statement. When moist air is forced to rise over a mountain or other high terrain, it cools and releases precipitation on the windward side. As the air mass descends on the leeward side, it warms and dries out, creating a rain shadow where little precipitation falls.

Rain Shadows Develop on the Leeward Side of Topographic Barriers