As air temperatures increase, evaporation increases, leading to more condensation and cloud formation. Low, thick cloud cover increases the albedo of the atmosphere, thereby having a cooling effect on Earth. This is an example of a

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This is an example of a negative feedback loop because the increase in cloud formation due to increased evaporation leads to a cooling effect on Earth, which ultimately inhibits further temperature increase.

As Air Temperatures Increase, Evaporation Increases, Leading to More Condensation