Precipitation is defined as water in liquid or solid forms falling to the earth.
It happens when continuous condensation in the body of air helps the water droplets or ice crystals to grow in size and weight that the air cannot hold them and as a result these starts falling on the ground under the force of gravity.
Forms of precipitation
The precipitation falls on the earth in various forms of droplets of water, ice flakes and solid ice balls or hail and at times droplets of water and hail together.
The form that precipitation takes is largely dependent upon the method of formation and temperature during the formation.
The forms of precipitation are as follows:
 Drizzle and Rainfall
Drizzle is a fairly uniform precipitation composed exclusively of fine drops of water with diameter less than 0.5 mm.
Only when droplets of this size are widely spaced is called rain.
When condensation takes place below freezing point, the water vapour changes into tiny ice crystals.
These tiny ice crystals grow in size and form ice flakes which become big and heavy and start falling on the ground.
This form of precipitation is called snowfall.
Snowfall is very common in Western Himalaya and mid and high latitude regions in winter.
Sleet is frozen rain, formed when rain before falling on the earth, passes through a cold layer of air and freezes.
The result is the creation of solid particles of clear ice.
It’s usually a combination of small ice balls and rime.
Hail is precipitation of small balls or pieces of ice (hail stones) with diameters ranging from 5 to 50mm, falling either separately or agglomerated into irregular lumps.
Hailstones are comprised of a series of alternating layers of transparent and translucent ice.