They will fall to the ground as snow.If the air is warmer than 0 degrees celsius , the ice crystals will melt.
some of it would defrost. then for every (umm) second that the snow is there another couple of thousand flakes melt.
Snow a falls down a the mountain!
snow
Sleet does not form in clouds - it begins as snow. The snow falls through a layer of air a little above freezing and melts into rain, then falls into a colder layer again and refreezes into ice pellets.
When the Snow Falls was created in 1985-01.
It evaporates into a second layer
some of it would defrost. then for every (umm) second that the snow is there another couple of thousand flakes melt.
a lot of snow falls
Sleet starts as snow, then falls through a layer of the atmosphere that is above freezing whereupon it melts into rain. Finally, it falls back into colder air and refreezes as ice pellets (sleet) before reaching the ground.
When snow falls through humid air that is close to freezing, the snowflakes tend to join together into larger clumps in which the individual crystals are hard to see. Powdery snow is produced when snow falls through cold dry air
snow falls down the mountain
If too much rain falls you will have tons of floods. If too much snow falls at once it will become a blizzard.
It melts, partially or totally. If the air remains above freezing the remainder of the way down to the ground, you'll get rain. If there is a sufficient cold layer below the layer of warm air down to the surface, it has time to refreeze into sleet. If there is a very shallow layer of sub-freezing air at the surface, rain will fall but freeze to the surface upon contact.
When snow falls through humid air that is close to freezing, the snowflakes tend to join together into larger clumps in which the individual crystals are hard to see. Powdery snow is produced when snow falls through cold dry air
Snow a falls down a the mountain!
cumulonimbus clouds
Ice pallet are also known as 'Sleet' -Its the solid form of water. They are formed when snow falls through a warm layer of air, partially melting, and then falls through a layer of air below 0*C. The resulting beads of ice are hard enough to bounce off the cold ground when they strike it.