The layers, however, do not occur simply due to the hailstone going through up and down cycles inside a thunderstorm. The conditions experienced by the hailstone can change as it passes horizontally across or near an updraft. Hailstones can have layers of clear and cloudy ice if the hailstone encounters different temperature and liquid water content conditions in the thunderstorm. The hail falls when the thunderstorm's updraft can no longer support the weight of the hailstone, which can occur if the stone becomes large enough or the updraft weakens. However, if the water freezes slowly, the air bubbles can escape and the new ice will be clear. If the water freezes instantaneously when colliding with the hailstone, cloudy ice will form as air bubbles will be trapped in the newly formed ice. Hailstones then grow by colliding with liquid water drops that freeze onto the hailstone’s surface. How does hail form? Hailstones are formed when raindrops are carried upward by thunderstorm updrafts into extremely cold areas of the atmosphere and freeze.
What we do: Read more about NSSL's hail research here. Hail can damage aircraft, homes and cars, and can be deadly to livestock and people. Watch on the NOAA Weather Partners YouTube Channel» What is hail? Hail is a form of precipitation consisting of solid ice that forms inside thunderstorm updrafts.
0 kommentar(er)
