Why is the east coast of India more prone to tropical cyclones than the west coast? Explain the post-monsoon (October–December) cyclone season.
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 →India's east coast faces far more tropical cyclones than its west coast. Between 1891 and 1990, about 262 cyclones struck a 50-km strip along the east coast, against 33 on the west coast [1]. The cause is both oceanic and geographical, and the risk is highest in the post-monsoon months.
Why the east coast is more prone
- More systems form in the Bay: the Bay of Bengal produces roughly four times as many cyclones as the Arabian Sea [1]. In October–December 1971–2020 it produced 168 depressions against 62 in the Arabian Sea [2].
- Warm, low-salinity surface water: freshwater from the Ganga–Brahmaputra stays on top and keeps the surface warm, which feeds convection.
- Pacific remnants: typhoon remnants from the South China Sea often regenerate over the Bay.
- Storms head for the coast: 81.5% of Bay systems cross the coast, against 32.3% for the Arabian Sea, where most dissipate at sea [2].
- Funnel-shaped Bay, shallow shelf, flat deltas (Krishna–Godavari, Mahanadi): these amplify storm surge, the main cause of cyclone deaths [1].
- West coast is sheltered: the Arabian Sea is cooler, and its storms usually track west or northwest, away from India.
The post-monsoon (October–December) season
- Trigger: the SW monsoon withdraws and northeasterly winds set in over the Bay [3]. The monsoon trough moves south over warm water, and vertical wind shear is low during this changeover.
- Systems form further south as the season goes on: depressions form at about 13.9°N in October and about 7.7°N in December [2]. Landfall therefore moves from Odisha and Andhra Pradesh to Tamil Nadu and Sri Lanka.
Oct: ~13.9°N → Odisha/AP | Nov: ~11.1°N → AP/TN | Dec: ~7.7°N → TN/Sri Lanka
Southward shift of where depressions form, Oct–Dec [2]
- Paths are hard to predict: in October 1976 a storm expected to hit Madras turned north to Masulipatnam. Madras still received 344 mm in four days [4].
- Mixed effect on rainfall: Tamil Nadu gets 48.1% of its annual rain in October–December [2], so these systems matter. But a storm can also pull moisture away: VSCS Hamoon (2023) cut Tamil Nadu's rainfall [5].
To sum up, warm seas, more systems forming and storms that head for the coast make the east coast India's main cyclone zone, and October–December is its peak season. IMD's day-wise forecasts [3] should be backed by surge-resilient shelters and last-mile warnings, in line with the Sendai Framework and SDG 11.
Sources
- 1NDMA – Cyclone (Natural Hazards)262 vs 33 cyclones (1891–1990); Bay has about 4× the Arabian Sea's cyclones; storm surge is the main killer
- 2Raj et al., "Understanding and prediction of Indian Northeast Monsoon over the years", MAUSAM 76(1), IMD, 2025168 vs 62 depressions; 81.5% vs 32.3% coastal crossing; formation latitudes for Oct–Dec; Tamil Nadu's 48.1% share of annual rain
- 3IMD Press Release, 15 October 2026SW monsoon withdrawal, northeasterly winds and NE monsoon onset; day-wise warnings
- 4The Hindu, "50 years ago: Cyclonic storm likely to cross A.P. coast to-day" (19 Oct 2026, Chennai edn., p. 13)1976 storm turned north to Masulipatnam; 344 mm at Madras
- 5IMD Chennai, Report on Northeast Monsoon 2023Hamoon reduced Tamil Nadu's rainfall