Hail is a form of solid precipitation often confused with Ice Pellets (Sleet). It consists of balls or asymmetrical layers of ice, each of which is called a hailstone. Hail forms in strong thunderstorm clouds, particularly those with intense updrafts, great vertical ,high liquid water content,extent, large water droplets, and where a good portion of the cloud layer is below freezing. These types of strong updrafts can also indicate the presence of a tornado. The growth rate of hailstones is impacted by factors such as higher elevation, lower freezing zones, and wind shear. Hail can range in size from a sphere comparable to a pea, all the way to the size of a grapefruit. Hail causes about $1 billion dollars in damage to property every year.
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