How does water cycle contribute to condensation?
Condensation if part of the water cycle and is what creates clouds
Condensation is one of the steps in the water cycle. It occurs after evaporation (when sunlight and other factors cause water vapour to rise into the atmosphere) and is what creates clouds.
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Condensation occurs in the water cycle when water vapor in the atmosphere cools and changes back into liquid form. This typically happens when warm, moist air rises and cools as it encounters cooler temperatures higher in the atmosphere or when it comes into contact with a cooler surface. As the air cools, it cannot hold as much water vapor, leading to the condensation of water droplets. The water cycle contributes to condensation by constantly replenishing the atmosphere with water vapor through processes such as evaporation from bodies of water, transpiration from plants, and sublimation from ice and snow. When the air becomes saturated with moisture, condensation occurs, resulting in the formation of clouds, fog, dew, or precipitation.
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When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
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