Physical Geography
Hail is a form of precipitation that consists of balls or irregular lumps of ice, known as hailstones, which fall from cumulonimbus clouds during thunderstorms. It typically forms when updrafts in these storms carry water droplets high into the atmosphere, where they freeze and accumulate layers of ice before falling to the ground. The size of hailstones can vary significantly, influenced by the strength of the storm's updrafts and the duration of their formation.
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