Rain is a type of precipitation consisting of liquid water droplets that have condensed from atmospheric water vapor and fall to the Earth's surface due to gravity.
Rain occurs when water droplets in the atmosphere become large and heavy enough to overcome air resistance and fall from clouds to the ground under the force of gravity.
Rain formation begins with evaporation, where water from oceans, lakes, rivers, and even soil transforms into invisible water vapor. This warm, moist air rises into the atmosphere. As it ascends, the surrounding air becomes cooler, causing the water vapor to condense into tiny liquid droplets. These droplets cluster together to form clouds. When they grow large enough through further condensation and collision, they fall as rain.
Not all liquid precipitation qualifies as rain. Several criteria must be met:
Raindrops have sizes ranging from 0.5 to 9 mm (0.0039 to 0.3543 in) mean diameter but develop a tendency to break up at larger sizes. Smaller drops are called cloud droplets, and their shape is spherical. As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow.
Rain is often classified based on intensity and duration:
Published:
May 1, 2025
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