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Hail is possible within most thunderstorms as it is produced by cumulonimbi, and within 2 nautical miles (3.7 km) of the parent storm. Hail formation requires environments of strong, upward motion of air with the parent thunderstorm (similar to tornadoes) and lowered heights of the freezing level.ny thunderstorm which produces hail that reaches the ground is known as a hailstorm. Hail has a diameter of 5 millimetres (0.20 in) or more. Hailstones can grow to 15 centimetres (6 in) and weigh more than 0.5 kilograms (1.1 lb). Unlike ice pellets, hailstones are layered and can be irregular and clumped together.
hail can form in 2 specific kind of thundercloud's. for the `usual` hail, it forms in a Cumulonimbus after the evaporated water condenses and falls. it frees-es in one of th â¦ e lower lairs of the thundercloud. it can reach different sises, depending in what area it formed.