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This naturally occurring process causes 2 different climates on opposite sides of a mountain:​

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The process that causes two different climates on opposite sides of a mountain is called orographic precipitation. This occurs when moist air is forced to rise over a mountain, causing it to cool and condense into clouds and rain. The side of the mountain facing the wind will receive more precipitation, while the side facing away from the wind will be drier. This can create two distinct climates on either side of the mountain, with one side receiving more rain and having a cooler climate, while the

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