Cloudburst Disasters in India: Causes and Policy Gaps
Why in the news
Cloudbursts across Himalayan states exposed weak climate readiness and early warning.
Key facts
- Threshold: above 100 mm per hour over roughly 30 sq. km.
- Typical in Himalayan regions where monsoon winds, cold winds and terrain interact.
- Effects spread: landslides, flash floods, downstream damage.
- Global warming and shifting monsoon raise frequency and intensity.
Challenges
- Drainage: urban flooding in Delhi, Mumbai and Bengaluru shows poor planning.
- Data gaps: small affected areas lack rain gauges; IMD lacks dense networks for hyper-local forecasts.
- Preparedness: fragile slopes face unregulated building and tourism.
Way forward
- Strengthen IMD with dense instruments and computing power.
- Map vulnerable zones with satellite imagery and past data.
- Coordinate IMD, scientists, planners and authorities.
- Upgrade drainage, regulate construction, reach communities with warnings.
Exam angle
- Definition threshold of a cloudburst.
- Forecasting agency: IMD.