Hail is a type of precipitation consisting of spheres of sleet covered with a crust of ice. Hailstones can be from 5 mm to 20 cm in diameter. For humans, hail is dangerous in several ways:
We have gathered the most important hail facts in this article! Go and read it whole now!
During a storm, storms throw raindrops into the very cold parts of the atmosphere, causing frost and hail to form. After that, it comes into contact with liquid droplets that freeze on the filled surface. The sudden freezing of water during hail storms creates dark ice in the form of bubbles trapped in the newly formed ice. However, when the water freezes slowly, bubbles escape and new ice becomes transparent. When the approaching storm becomes unbearable, it rains hail. This could be due to the rock being big enough or the depletion being weak. Do you want to know more hailstorm facts, don’t you?! Go ahead!
If hail is exposed to varying temperatures and conditions of liquid water content during a thunderstorm, the hail can have a clear, cloudy layer of ice. The conditions encountered by hail can change if the hail is horizontal in or near an updraft. However, layers are not only created by hail that circulates up and down in a thunderstorm. The wind in a thunderstorm is not limited to the top and bottom. Interesting hail facts waiting for you below.
Horizontal winds come from rotating updrafts like a supercell storm or horizontal winds from the area. Hailstones do not grow even in a storm. At very high altitudes, the air is cold enough (less than -40 ° F) and all liquid water turns to ice. Hailstones require liquid water to grow to a substantial size.
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The easiest way to convey the size of the hail is to compare it to your everyday ones. An inch of hail is about a quarter the size of the United States. 1.5 inches of hail is the size of a ping pong ball. When it reaches 1.75 inches in diameter, it is called a golf ball size hail. This is a very dangerous case. Baseball-sized hail sounds like sparks when hitting at 2.75 inches in diameter and large enough to fit a hole in the floor. When you reach the size of a grapefruit (4″) or softball (4.5″), you need to head underground until there is a storm. Fortunately, these samples are rare.
Major grapefruit hail storms or major hail storms are responsible for only 0.5% of all hail recorded in the last 60 years.
In July 2010, there was the worst snowfall ever in a small town in South Dakota. He crashed into Vivian, was eight inches tall, and weighed about two pounds. For some, it’s the size of a volleyball. The supercell that produced the pistachios created a small hurricane that blows at a speed of 80 km / h.
How does hail fall to the ground?When it becomes heavy enough to overcome the rising force of a thunderstorm, hail will fall and gravity will be pulled to the ground. These are very important scientific facts about hail. Large hail is usually closer to a rising outflow than a small hail because small hail can be blown by a current rising due to horizontal winds. If the wind near the surface is strong enough, the hail can fall diagonally or almost sideways! Hail can tear down the side tracks of a house, smash windows and blow away the house, smash the windows on the sides of the car, and cause serious injuries or death to people or animals.
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