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The eastern side of the Sierra Nevada and Cascades experiences drying primarily due to the rain shadow effect. As moist air from the Pacific Ocean rises over the mountain ranges, it cools and loses moisture in the form of precipitation on the western slopes. By the time the air descends on the eastern side, it is much drier, leading to arid conditions and limited rainfall in that region. This phenomenon creates a stark contrast in vegetation and climate between the western and eastern flanks of these mountain ranges.

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4w ago

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