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When warm moist winds blow inland from the ocean toward a coastal mountain range the winds are forced upward over the mountains as these warm winds rise the air cools and the moisture falls out as precipitation. This is called orographic precipitation, or orographically-enhanced precipitation.

On the other side of the mountain, the air descends and warms, drying it out as the precipitation ends. This side of the mountain can be markedly dryer, and is called the Rain Shadow.

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