Meteorology
Hail is a type of solid precipitation that consists of balls or irregular lumps of ice, known as hailstones, which form in thunderstorms with strong updrafts. The process of hail formation involves the repeated cycling of water droplets within a storm cloud, allowing them to freeze and accumulate layers of ice before falling to the ground. This phenomenon is closely tied to various meteorological processes, particularly in the context of severe weather events.
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