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Q: When hailstones are repeatedly blown back into the atmosphere?
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How are sleet and hailstones formed diffrently?

Sleet is formed when ice crystals fall as rain that freeze before it hits the ground. Hailstones form when strong winds blow raindrops back upward to the top of where the temperature is freezing. Then, the raindrops freeze into small pieces of ice. This process might happen several times where many layers of ice may build up. Once the hailstones are too heavy and the wind can blow them back up, the hail falls to the ground.


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How do large hail stones grow?

As small sized hailstones get lower in the weather system, they may be driven back upwards by the wind, and are enlarged by being added to by further ice. Eventually, they will fall to earth, and may cause damage due to their larger size.


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How are hailstones made?

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.


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Why are hailstones big as a baseball?

Most are not. Most hailstones are pea to marble sized. A hailstone can only get to a certain size of the thunderstorm has a strong enough updraft to hold it airborne. If a storm is dropping baseball sized hail, then that means the air in the storm is moving up at a fast enough rate to hold the hailstones until they get that big. This suggests air is moving up at over 100 mph.


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