Corn Crop after hail storm |
Hail is formed in huge cumulonimbus clouds, commonly known as thunderheads. The development of hail starts inside a thunderstorm. Where there are strong updrafts of warm air and downdrafts of cold air. If water droplets are present the can be carried to the freezing level with temperatures that reach below 32F and the droplets will freeze. The frozen droplets are carried by the cold downdrafts and as it travels downward it may melt into warmer air toward the bottom of the thunderstorm. A repetition of the frozen droplet being carried up by an updraft and taken to the freezing level will add another layer of ice which creates HAIL. With the several layers the ice, the hail fall to the ground.
The size of hail is not so different from a raindrop. Mostly hail is 2inches in diameter or less. The largest hailstone fell on June 23, 2003 in Aurora, Nebraska and had a diameter of 7.0 inches, a circumference of 18.75 inches, and weighed just under 1 lb. The heaviest hailstone fell in Coffeeville, Kansas on September3, 1970 and weighed 1.67 lbs. It had a diameter of 5.7 inches and a circumference of 17.5 inches.
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