Precipitation occurs in the atmosphere when water vapor condenses into droplets or ice crystals that become heavy enough to fall to the ground due to gravity. This process is typically facilitated by cooling of air, which can happen as air rises and expands in the atmosphere. Factors such as temperature, humidity, and atmospheric pressure play crucial roles in the formation of clouds and the subsequent release of moisture. Common forms of precipitation include rain, snow, sleet, and hail, depending on temperature conditions.
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