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Height above sea level, or elevation, can impact climate in a few ways. As elevation increases, the temperature tends to decrease, because the air is thinner and can't hold heat as effectively. Additionally, higher elevations may receive more precipitation due to orographic effects, where moist air is forced to rise and cool, leading to condensation and rainfall or snow. Finally, high elevations may also experience more intense sunlight and stronger UV radiation due to their proximity to the sun.

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