A hailstorm is a type of precipitation in which ice pellets (hailstones) fall from the sky during thunderstorms, especially from Cumulonimbus Clouds.
- They are most common in the midlatitudes.
Conditions For Formation
- Presence of intense thunderstorms
- Strong vertical air currents (updrafts)
- Freezing temperatures at upper levels
- High moisture content
Hailstorm Forming Process
- Hail forms inside Cumulonimbus Clouds, which are tall clouds with strong winds.
- Strong upward winds (updrafts) carry tiny water droplets high into the cloud.
- At high altitude, temperature is very low → droplets freeze into small ice particles.
- These ice particles move up and down inside the cloud and collect more water → layers of ice form.
- Hailstones keep growing as more ice is added.
- When they become too heavy for the updraft to hold, they fall as hailstones.
Impact
- Crop damage , infrastructure damage and loss of lives.

Source: Down To Earth