soft hail
Quick Summary
Soft hail, also known as graupel, is a type of precipitation. It consists of white, opaque, rounded or conical pellets with a diameter of up to 6 mm (0.2 inch). These pellets are formed from small cloud droplets that have frozen together, giving them a low density. Soft hail is readily crushed and is distinct from small hail (ice grains) and true hailstones, which are larger and often have layered structures of clear and opaque ice. Soft hail can be associated with thunderstorms.123
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- climateHail
The first is soft hail, or snow pellets, which are white opaque rounded or conical pellets as large as 6 mm (0.2 inch) in diameter. They are composed of small cloud droplets frozen together, have a low density, and are readily crushed.
Read MoreThe first is soft hail, or snow pellets, which are white opaque rounded or conical pellets as large as 6 mm (0.2 inch) in diameter. They are composed of small cloud droplets frozen together, have a low density, and are readily crushed.
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atmospherePrecipitation of ice…or less spherical particle called graupel. Smaller-sized graupels are generally referred to as snow grains. In cumulonimbus clouds during conditions where graupels are repeatedly wetted and then injected back toward high altitudes by strong updrafts, very large graupels called hail result. Hail has been observed on the ground at sizes…
Read More…or less spherical particle called graupel. Smaller-sized graupels are generally referred to as snow grains. In cumulonimbus clouds during conditions where graupels are repeatedly wetted and then injected back toward high altitudes by strong updrafts, very large graupels called hail result. Hail has been observed on the ground at sizes…
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