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Rapidly cooling temperatures can significantly affect the water cycle by increasing the rate of condensation and precipitation. As air cools, it holds less moisture, leading to the formation of clouds and potentially more intense rainfall or snowfall. Additionally, lower temperatures can lead to increased evaporation from bodies of water, but this effect may be overshadowed by the condensation process. Ultimately, these changes can disrupt local weather patterns and influence ecosystems reliant on stable water supply.

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