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Orographic clouds form when moist air is forced to rise over a mountain range. As the air ascends, it cools, leading to condensation and the formation of these clouds, which are the source of orographic precipitation, such as rain or snow. This precipitation primarily falls on the side of the mountain facing the prevailing wind. Areas on the leeward side of the mountains often experience significantly less precipitation, creating a "rain shadow". Orographic clouds are a specific type of cloud formation resulting from air being lifted by topography.12

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