by the force of strong upward air currents
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.
Hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. The storm's updraft blows the hailstones to the upper part of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted up again. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud. In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones.
There are many reasons why fog droplets remain suspended in the air. These droplets are not heavy enough to fall.
Water vapor form snowflakes when the temperatures in the air are above freezing and the air should be unsaturated. The water vapor to create hailstones start inside a cumulonimbus cloud and super cooled liquid water are caught in a strong updraft. The cycle continues to increase the size of the hailstone, then eventually falls to the earth's surface.
they are supported by slight movements of the air
It is called hailstones or ice.
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.
Hail forms in storm clouds when supercooled water droplets freeze on contact with condensation nuclei, such as dust or dirt. The storm's updraft blows the hailstones to the upper part of the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted up again. The hailstone gains an ice layer and grows increasingly larger with each ascent. Once a hailstone becomes too heavy to be supported by the storm's updraft, it falls from the cloud. In large hailstones, latent heat released by further freezing may melt the outer shell of the hailstone. The hailstone then may undergo 'wet growth', where the liquid outer shell collects other smaller hailstones.
What your looking for is this word Megacryometeorhave a look at this pagehttp://en.wikipedia.org/wiki/MegacryometeorAlso check out hale, hailstones
A cloud.
Cloud
There are many reasons why fog droplets remain suspended in the air. These droplets are not heavy enough to fall.
Cumulonimbus clouds have a large and tall horizontal appearance. They are capable of producing severe weather conditions such as thunderstorms and hailstones.
Cloud.
A wall cloud is suspended from a cumulonimbus cloud (mostly during thunderstorms). Then the wall cloud begins rotating counter-clockwise. Then a funnel cloud will drop from it.
Hailstones is the correct answer please email me at danielletrokey@ymail.com if this helped u r not. Thanks
Cloud Formation.