The dry leeward side of a mountain is often termed a (n)

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The term for the dry leeward side of a mountain range is commonly referred to as the rain shadow. As moisture is forced to rise on the windward side of a mountain range, it releases precipitation, leaving little moisture left to fall on the leeward side. This results in a much drier climate on the opposite side of the mountain range, known as the rain shadow. Choices B, C, and D are not accurate in describing the dry leeward side of a mountain range.

The Dry Leeward Side of a Mountain Is Often Termed