Answer:
Precipitation:
rain - a liquid type, occurs when water droplets in clouds start to collide with each other and stick together, which forms bigger drops, and once they get too big, gravity cannot support them, causing them to fall to the ground.
snow - Snow really happens pretty much every time it downpours, yet the snow regularly liquefies before it arrives at the ground. There is a form of virga created by snow called fallstreaks. Fallstreaks are regularly seen with high, wispy cirrus mists. However snow all the more effectively falls through sub-freezing air, it is workable for snow to fall in any event, when the air temperature is above freezing.
sleet - Slush and freezing precipitation happen under very much like conditions. Slush is pellets of ice that structure when snow falls into a warm layer and melts into the downpour. The downpour then, at that point, falls into a freezing layer of air that is sufficiently profound to refreeze the raindrops into pellets. Now and then the snow doesn't totally liquefy and to some degree liquefied snowflakes refreeze into snow pellets. Freezing precipitation happens when snow falls into a warm layer and melts, however, the freezing layer is exceptionally shallow, so the fluid water falls onto surfaces that are underneath freezing and sets, bringing about an in any event, covering of ice on roads, trees, vehicles, and electrical cables.
hail - Hailstones are enormous lumps of ice that tumble from huge tempests. They are exceptionally harmful to crops, effectively acquiring the epithet "the white plague". Vicious rainstorms have exceptionally solid updrafts that are sufficiently able to hold ice high up against the draw of gravity. In Figure B, you can see that a hailstone has layers like an onion. The obscure layers are made when the hail is in the colder segment of the cloud or gets found out in the downdrafts, and the supercooled drops freeze onto the hail so rapidly little air bubbles get caught, making the ice look smooth. At the point when the hail falls into the hotter piece of the cloud, or into the warm updrafts, the supercooled drops freeze gradually sufficient that the minuscule air has the opportunity and willpower to escape before the water freezes, bringing about a sheet of clear ice. Hail can go in size from the distance across of a pea to bigger than a grapefruit. Hail the size of grapefruits has been known to cause broad property harm and even fatalities. However, even little hail can make harm harvests and injury or imprint them, diminishing their worth.
hope this helps!