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Evaporating water vapor rises to high altitudes, where the temperature is low enough for the vapor to condense back into liquid water. Generally the vapor condenses around small particles of dust. The technique of cloud 'seeding' introduces small particles into clouds to facilitate the formation of raindrops.

Air currents raise the falling drops over and over. They get bigger and bigger, until they are too heavy to rise on the currents, and then they fall to earth.

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