Hail
Hail is a type of graupel (a form of precipitation) composed of spears or irregular lumps of ice. It occurs when supercooled water droplets (remaining in a liquid state despite being below the freezing point, 0 °C/32 °F) in a storm cloud aggregates around some solid object, such as a dust particle or an already-forming hailstone. The water then freezes around the object. Depending on the wind patterns within the cloud, the hailstone may continue to circulate for some time, increasing in size. Eventually, the hailstone falls to the ground, when the updraft is no longer strong enough to support its weight.
Hail can do serious damage, notably to automobiles, skylights, and glass-roofed structures. Rarely, massive hailstones have been known to cause concussions or fatal head trauma.
Hailstones, while most commonly only a few millimetres in diameter, can sometimes grow to several centimetres or occasionally even bigger. Pea or golfball-size hailstones are not uncommon in severe storms. The image to the right shows an aggregate hailstone with smaller stones visible. The ruler shows the size of this hailstone as approximately 6 cm, almost the size of a tennis ball.
Costly or Deadly Hailstorms
July 11 1990, Denver, Colorado, USA, $625 million, softball-sized hail destroyed roofs and cars
May 5 1995, Dallas and Fort Worth, Texas, USA, $2 billion
April 12 1999, Sydney, New South Wales, Australia, $190 Million. 15 thousand homes lost power and several people were injured.
July 19 2002, Henan Province, China, 25 dead and hundreds injured
da:Hagl
de:Hagel
es:Granizo
eo:Hajlo
fr:Grêle
it:Grandine
he:ברד
nl:Hagel
ja:霰
pl:Grad
sv:Hagel
th:ลูกเห็บ