hailstone
Quick Summary
Hail is a form of precipitation consisting of balls or pieces of ice with diameters ranging from 5 mm (0.2 inches) to over 15 cm (6 inches). It typically forms in cumulonimbus clouds with strong updrafts, often accompanying thunderstorms. Large hailstones can have alternating layers of clear and opaque ice due to varying freezing rates. Hailstorms are most common in mid-afternoon in the mid-latitudes and usually last about 15 minutes. Hail can be extremely destructive to buildings, crops, and livestock.12
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- climateShowers, thunderstorms, and hail
The hailstones that fall from deep, vigorous clouds in warm weather consist of a core surrounded by several alternate layers of clear and opaque ice. When the growing particle traverses a region of relatively high air temperature or high concentration of liquid water, or both, the…
Read MoreThe hailstones that fall from deep, vigorous clouds in warm weather consist of a core surrounded by several alternate layers of clear and opaque ice. When the growing particle traverses a region of relatively high air temperature or high concentration of liquid water, or both, the…
Read More - climateHail
True hailstones, the third type, are hard pellets of ice, larger than 5 mm (0.2 inch) in diameter, that may be spherical, spheroidal, conical, discoidal, or irregular in shape and often have a structure of concentric layers of alternately clear and opaque ice. A moderately severe…
Read MoreTrue hailstones, the third type, are hard pellets of ice, larger than 5 mm (0.2 inch) in diameter, that may be spherical, spheroidal, conical, discoidal, or irregular in shape and often have a structure of concentric layers of alternately clear and opaque ice. A moderately severe…
Read More