As per IMD definition, over 100 mm of rainfall in one hour is called a cloudburst. It usually occurs over a small geographical region (20-30 sq.km).
Mechanism of Cloudbursts:
- In India, cloudbursts often occur during the monsoon season, when the south-westerly monsoon winds bring in copious amounts of moisture inland. The moist air that converges over land gets lifted as they encounter the hills.
- The moist air reaches an altitud eand gets saturated, and the water starts condensing out of the air forming clouds.
- Such an orographic lifting together with a strong moisture convergence can lead to intense cumulonimbus clouds taking in huge volumes of moisture that is dumped during cloudbursts.
- Tall cumulonimbus clouds can develop in about half an hour as the moisture updraft happens rapidly, at a pace of 60 to 120 km/hr.
Occurrence of Cloudbursts:
Cloudbursts, hence, occur mostly over the rugged terrains over the Himalayas, the Western Ghats, and north-eastern hill States of India. The heavy spells of rain on the fragile steep slopes trigger landslides, debris flows, and flash floods causing large-scale destruction and loss of people and property.
IMD is enhancing its automatic weather stations, government will give hourly data that can help map cloudburst-prone regions. Multiple doppler weather radars can monitor moving cloud droplets and help to provide forecast for next three hours.