the heaviest hailstone on record fall was.... 1130
The heaviest hail on record (currently) is 132 grams.
Hailstones form inside thunderstorm clouds when supercooled water droplets freeze onto ice nuclei. As the hailstones grow, they eventually become too heavy for the updrafts in the storm to support, causing them to fall to the ground.
Hailstones are formed in thunderstorms when updrafts carry raindrops into extremely cold regions of the atmosphere, where they freeze into ice pellets. As the hailstones are lifted and fall repeatedly within the storm, they accumulate layers of ice until they become heavy enough to fall to the ground as hail.
== == Hailstones are raindrops that freeze as they fall through layers of very cold air. When they fall down from the sky hailstones are usually as big as peas. Sometimes they can be as big as tennis balls - so watch out!
Hailstones start off as a snowflake. In order to become a hailstone, a upwind has to blow it back up into the cloud and collect more water, snow, or ice. Then it freezes. This process can happen over and over again until the hailstone is heavy enough to fall out of the cloud. That's the process of a hailstone.
Hailstones remain suspended in a cloud due to the strong updrafts present within the cloud. As the hailstones are being formed, they are continuously lifted higher into the colder regions of the cloud by these updrafts. This cycle repeats until the hailstones become too heavy and fall to the ground as precipitation.
The Midwest of the United States
because they are frozen rain drops
Hailstones kill people by fall in far from the sky and falling faster till it will do damage to the cerebrum.
Hail forms in strong thunderstorms with intense updrafts. As water droplets are lifted high into the cloud, they freeze and collect layers of ice. When they become too heavy for the updrafts to support, they fall to the ground as hailstones. The size of the hailstones depends on the strength of the updrafts and the amount of moisture in the cloud.
Large hailstones are formed within strong thunderstorm clouds, particularly those with intense updrafts. As water droplets are lifted high into the atmosphere, they freeze and accumulate layers of ice as they are carried upward and downward within the storm. The repeated cycling through the cloud allows hailstones to grow larger until they become too heavy for the updrafts to support, resulting in their fall to the ground as hail. Factors such as the strength of the updraft and the moisture content in the atmosphere play crucial roles in the size of the hailstones.
Hailstones grow in thunderstorms through a process called accretion. As updrafts carry water droplets high into the cold upper atmosphere, these droplets freeze and form ice pellets. As the pellets are lifted and dropped multiple times within the storm, they collect additional layers of water that freeze upon contact, causing the hailstones to grow larger. Eventually, when they become too heavy for the updrafts to support, they fall to the ground as hail.