Why does the Bay of Bengal generate more intense post-monsoon cyclones than the Arabian Sea? Discuss their implications for coastal States.
New · District CollectorCan you hold the district for 72 hours?Floods, a heatwave, an outbreak, a grievance queue. Take the decisions, see the consequences.Play →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
- 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
- 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
- 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
- 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