·The Hindu·15 marks·250–350 words

Why does the Bay of Bengal generate more intense post-monsoon cyclones than the Arabian Sea? Discuss their implications for coastal States.

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In this answer
  1. Why the Bay of Bengal generates more intense cyclones
  2. Implications for coastal States

The Bay of Bengal produces roughly four cyclones for every one in the Arabian Sea [1], and its post-monsoon (October–December) storms are often the strongest of the year. Cyclone Arnab fits this pattern. It was a Very Severe Cyclonic Storm that triggered a red-message warning for Andhra Pradesh and south Odisha in October 2026 [2]. The ocean, the atmosphere and the shape of the coast together explain the difference.

Why the Bay of Bengal generates more intense cyclones

  • Warmer sea: The Arabian Sea is relatively colder, which holds back cyclone formation and intensification. The Bay stays warm enough to keep feeding storms [1].
  • Pacific remnants: Remnants of north-west Pacific typhoons move west over South-East Asia and strengthen again over the Bay [1].
  • Freshwater layer: Monsoon rain and Ganga–Brahmaputra discharge leave a low-salinity surface layer. It resists mixing, so storms do not stir up cooler water from below.
  • Post-monsoon atmosphere: As the monsoon retreats, wind shear weakens. Arnab was expected to intensify further as it detached from the ITCZ [2].
  • Arabian Sea handicaps: Most Bay storms weaken over land and rarely cross into the Arabian Sea [1]. Drier air over the Arabian Sea also suppresses cyclones.

Implications for coastal States

  • Exposure: India has about 7,500 km of coastline, and about 40% of its population lives within 100 km of it [3]. The Bay's shallow shelf and funnel-shaped head raise storm surge in Odisha, West Bengal and Andhra Pradesh.
  • Economic loss: Even as deaths fall, losses rise: an estimated USD 4.2 billion from Fani and USD 14 billion from Amphan [3]. Crops, ports, fisheries and power networks are hit hardest.
  • Forecasting stress: For Arnab, IMD forecast winds of 115–125 km/h two days before landfall [2]. A storm that strengthens faster than forecast leaves less time to evacuate.
  • Resilience gains: NCRMP and related projects built 830 multi-purpose shelters and 33,258 resilient houses in coastal districts of AP, Odisha and Tamil Nadu [3]. Cyclone deaths fell by about 94% over two decades [3].
  • Persisting gaps: The Parliamentary Standing Committee on Home Affairs (2020) found that construction had not begun on some early-warning projects commissioned in 2015 [4].
  • Shifting risk: Cyclone frequency and intensity are rising over the Arabian Sea [3]. Gujarat, Maharashtra and Kerala therefore need east-coast-style preparedness.

The Bay's warm, stratified, Pacific-fed waters make it India's main cyclone hotspot, and a warming ocean raises the stakes. The next steps should be impact-based forecasting, sub-surface ocean monitoring by INCOIS, last-mile community warning and on-time NCRMP delivery. These would move coastal States from "zero casualty" towards "zero avoidable loss", in line with the National Disaster Management Plan, 2019 and SDG 13.

Sources

  1. 1RSMC New Delhi (IMD), Frequently Asked Questions on Tropical Cyclones and Marine Weather Services: the 4:1 Bay-to-Arabian Sea ratio, the colder Arabian Sea, north-west Pacific typhoon remnants, and Bay storms weakening over land
  2. 2IMD, Tropical Cyclone Advisory No. 07 (based on 1800 UTC, 26 Oct 2026): Arnab as a VSCS, the red-message warning for AP and south Odisha, the forecast of 115–125 km/h, and further intensification after detaching from the ITCZ
  3. 3World Bank, National Cyclone Risk Mitigation Project (Phase III) (P179725), Project Information Document: coastline and population exposure, Fani and Amphan losses, the 830 shelters and 33,258 houses, the 94% fall in deaths, and rising Arabian Sea activity
  4. 4PRS Legislative Research, Demand for Grants 2021-22 Analysis: Home Affairs: Standing Committee (2020) finding on early-warning projects in Odisha and AP that had not started

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