The air a few miles above the ground is always cold enough for water to freeze. Hail starts off as small pellets of ice called graupel in the cold, upper reaches od a thunderstorm. This graupel is cycled through the storm by powerful air currents. As this happens, the pellets collide with supercooled water droplets, in which water remains liquid below its normal freezing point. These droplets freeze instantly to the surface. Hailstones grow by accumulating layers of ice in the manner. Eventually the hail becomes too heavy to remains suspended in the storm and falls to the ground. The hail is large enough and falls fast enough that it does not have time to melt.
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Hail is formed when updrafts in a thunderstorm carry water droplets high into the atmosphere where they freeze into ice. As these ice pellets are lifted and fall through the storm, they can accumulate layers of frozen water before eventually falling to the ground as hail.
Hail is a solid form of precipitation which consists of lumps of ice that are individually called hailstones.
they are made from rain. as it falls it freezes causing ice but in the form of rain.
Ice crystals that fall from the sky are called snowflakes.
When strong winds toss ice crystals up and down in a cloud, it can lead to the formation of hail. As the ice crystals are carried up and down in the cloud, they encounter different temperature zones that cause them to grow larger. Eventually, the ice crystals become too heavy to be supported by the wind and fall to the ground as hail.
Cirrus clouds are primarily made out of ice crystals.
Cirrus clouds are composed primarily of ice crystals. They appear wispy and thin with a feathery or fibrous texture, often high in the atmosphere.
Clouds are not solid; they are made up of water droplets and ice crystals.