Atmospheric Science
Hail is a form of precipitation that consists of balls or irregular lumps of ice, which forms within strong thunderstorms. The development of hail is closely linked to the presence of intense updrafts in thunderstorms, allowing ice pellets to grow larger as they are carried upward and repeatedly coated with supercooled water before falling to the ground. This phenomenon is significant because it plays a crucial role in understanding different precipitation types, thunderstorm dynamics, severe weather impacts, and the overall behavior of storms in the atmosphere.
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