Orographic lifting involves moist winds meeting mountains, causing air to rise, cool, form clouds, and lead to precipitation.
Orographic lifting occurs when moist winds encounter mountains, forcing the air to rise and cool adiabatically, leading to cloud formation and precipitation. The windward side of the mountain receives more precipitation than the leeward side, known as the 'rainshadow effect.' One example of orographic lifting is the Sierra Nevada mountains, where moist air from the Pacific ocean results in significant rain on the western side and a dry desert on the eastern side.
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