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‘Mini-cloudbursts’ are on the rise

Basics

  • Cloudburst:
    • Sudden, extreme rainfall in a localized area (≥100 mm/hr over a few sq. km).
    • Common in hilly regions due to orographic lift and moisture-laden winds.
  • Mini-cloudburst:
    • Smaller in scale, but with intense rainfall (typically 50–100 mm/hr).
    • Increasingly reported in recent years.
  • Forecasting:
    • IMD states that cloudbursts remain impossible to forecast due to their highly localized and short-lived nature.
    • Mini-cloudbursts, though more frequent, are also hard to predict with current models.

Relevance : GS 3(Disaster Management – Floods , Cloudbursts, Environment – Climate Change)

Recent Rainfall Trends (2025 Monsoon till Aug 31)

  • Overall Monsoon (June–Aug 2025): 6% above normal (76.2 cm vs usual 70 cm).
  • Regional distribution:
    • Northwest India: +26% above normal (Uttarakhand, UP, Punjab, Haryana, J&K, Rajasthan, Delhi).
    • Central India: +8.6% above normal.
    • Southern Peninsula: +9.3% above normal; August rainfall (25 cm) = 3rd highest since 2001.
    • East & Northeast India: –17% deficit despite being the traditional rain-surplus zone.
  • September Outlook: Expected above normal rainfall (+9% vs average 16.7 cm), continuing a trend noticed since 1980.

Heavy Rainfall Episodes

  • August 2025:
    • 700+ instances of heavy rain (≥20 cm/day), 2nd highest since 2021 (behind 800+ in 2024).
    • Northern India: August rainfall = 26.5 cm, highest since 2001.
  • Drivers of extreme events:
    • Interaction between Western Disturbances (from Mediterranean) and Bay of Bengal storms → convergence of moisture → intense rain bursts.
    • Resulted in devastating floods and landslides in Himachal Pradesh, J&K, Uttarakhand.

Key Analytical Insights

  • Mini-cloudbursts on the rise:
    • May be linked to climate change-driven shifts: warming atmosphere holds more moisture, increasing probability of intense short-duration rainfall.
    • Urbanization + deforestation in hilly areas amplifies impacts (flash floods, landslides).
  • Changing monsoon dynamics:
    • September becoming wetter since 1980 (possibly due to delayed monsoon withdrawal + oceanic-atmospheric changes like Indian Ocean Dipole).
    • Regional inequality: Surplus in NW & Central India, deficit in East & NE → disrupts agriculture, hydrology, disaster preparedness.
  • Forecasting limitations:
    • While seasonal/weekly monsoon forecasts improving, sub-hourly localized predictions like cloudbursts remain beyond current radar and model resolution.
    • IMD using Doppler radars + AI-based nowcasting to reduce unpredictability.
  • Policy & Preparedness Implications:
    • Need for micro-level disaster management plans, especially in Himalayan states and urban flood-prone zones.
    • Resilient infrastructure + improved early warning systems essential.

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