·The Hindu·15 marks·250–350 words

Rapid intensification of tropical cyclones is challenging India's early-warning systems. Examine with reference to recent cyclones on the east coast.

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In this answer
  1. How RI strains early-warning systems
  2. Evidence from recent east-coast cyclones
  3. Gaps in the warning chain
  4. Way forward

Rapid intensification (RI) is a sharp rise in a cyclone's sustained winds within about a day. On IMD's scale, a storm can jump from Severe (48–63 kt) to Very Severe (64–89 kt) or higher before warnings catch up [2]. As the Bay of Bengal warms, RI is making warning lead-time the weakest link in India's cyclone management.

How RI strains early-warning systems

  • Intensity error: models forecast a storm's track better than its strength. If the forecast category is too low, fewer villages are evacuated.
  • Compressed lead-time: evacuation orders, fishing bans and shutdowns depend on the forecast category. RI leaves districts hours to act, not days.
  • Hidden ocean heat: satellites measure the sea surface, but the deeper warm water that feeds sudden strengthening is hard to observe.

Evidence from recent east-coast cyclones

  • Amphan (2020): it intensified rapidly over 24 hours and became the first Super Cyclonic Storm over the Bay since 1999 [3].
  • Arnab (2026): IMD forecast winds of 115–125 km/h, gusting to 140 km/h, for landfall day [1]. The storm reportedly grew stronger than some models predicted. It then crossed the Andhra coast hours early and at night, cutting short the evacuation window.

Gaps in the warning chain

  • Delayed infrastructure: a Parliamentary Standing Committee, cited by PRS, found that some early-warning projects for Odisha and Andhra Pradesh commissioned in 2015 had not started [4].
  • Last-mile alerts: under the World Bank-funded NCRMP-II, the siren target was cut from 750 to 200 [5]. Sirens matter most for a night landfall, when people are asleep.

Way forward

  • Plan for the worst plausible case: IMD and INCOIS should issue probabilistic intensity forecasts. Evacuation zones should be drawn for the upper category, not only the most likely one.
  • Better ocean data: feed sub-surface heat readings from buoys and Argo floats into intensity models.
  • Impact-based forecasting: target shutdowns to the zones most at risk, so warnings stay credible.
  • Community warning teams: Bangladesh's Cyclone Preparedness Programme has 76,000+ volunteers [6]. Its experience shows that trained villagers can act within a short warning window.

RI does not make India's zero-casualty model obsolete. It shifts the task from predicting a storm precisely to preparing for uncertainty. Combining better ocean science with community-led, last-mile warning, as the Disaster Management Act, 2005 and the Sendai Framework envisage, can protect the gains Odisha and Andhra Pradesh have made as the Bay warms.

Sources

  1. 1IMD, Tropical Cyclone Advisory No. 07 (based on 1800 UTC, 26 Oct 2026)Arnab forecast of 115–125 km/h gusting to 140 km/h
  2. 2RSMC New Delhi (IMD), Terminology on Cyclonic Disturbances over the North Indian OceanSCS and VSCS wind bands
  3. 3RSMC New Delhi (IMD), Press Release on Super Cyclonic Storm Amphanrapid intensification over 24 hours; first Bay of Bengal SuCS since 1999
  4. 4PRS Legislative Research, Demand for Grants 2021-22 Analysis: Home AffairsStanding Committee finding on stalled early-warning projects in Odisha and Andhra Pradesh
  5. 5World Bank, National Cyclone Risk Mitigation Project-II (P144726)siren target cut to 200
  6. 6UNDRR, Bangladesh: Advancing Early Warnings for AllCyclone Preparedness Programme has 76,000+ volunteers

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