Chapter 17 · 11 min read

Cyclones, Tropical Weather Systems & Disaster Risk Reduction

Overview

India is one of the world's most disaster-prone countries — exposed to 85% of its geographic area to one or more hazards. Cyclones and floods together account for the majority of India's disaster-related losses. Since the 1999 Odisha Supercyclone, India has transformed its disaster preparedness — reducing deaths dramatically even as cyclone intensity increases due to climate change.

For UPSC, this chapter sits at the heart of GS3 Disaster Management, GS1 Physical Geography (cyclone formation, monsoon weather systems), and is linked to GS2 (institutional frameworks — NDMA, SDMA). The Sendai Framework, NDMA, NDRF, and CDRI are high-frequency Prelims facts.

Key Fact: India is struck by ~10–12 tropical cyclones per year across the Bay of Bengal and Arabian Sea. The Bay of Bengal accounts for ~80% of India's cyclones. Arabian Sea cyclone intensity has increased 40% since 1982 (Nature Climate Change, 2021), driven by Indian Ocean warming.


Tropical Cyclone — Basics

What is a Tropical Cyclone?

A tropical cyclone is an organised rotating weather system that develops over warm tropical ocean water with sustained winds ≥63 km/h (Beaufort Scale 12). The same system is known by different names in different ocean basins:

BasinName
Indian Ocean (Bay of Bengal + Arabian Sea)Cyclone
Atlantic Ocean, Eastern PacificHurricane
Western PacificTyphoon
AustraliaWilly-Willy

Conditions for Formation

  1. Sea Surface Temperature (SST): ≥26–27°C to a depth of 60 m
  2. Atmospheric instability: Warm, moist air must rise and condense
  3. Coriolis effect: Minimum 5° latitude from equator (deflects winds; creates rotation)
  4. Low vertical wind shear: Upper-level winds must not be too different from lower-level winds
  5. Pre-existing disturbance: Low-pressure area or tropical wave as seed
  6. High relative humidity in middle troposphere (6–7 km altitude)

Why cyclones don't form on the equator: Coriolis force is zero at the equator — no rotation possible.

IMD Cyclone Classification

CategoryWind SpeedAcronym
Depression31–61 km/hD
Deep Depression52–61 km/hDD
Cyclonic Storm62–88 km/hCS
Severe Cyclonic Storm89–117 km/hSCS
Very Severe Cyclonic Storm118–167 km/hVSCS
Extremely Severe Cyclonic Storm168–221 km/hESCS
Super Cyclonic Storm≥222 km/hSUCS

Bay of Bengal vs Arabian Sea Cyclones

Why Bay of Bengal Produces More Cyclones

FactorBay of BengalArabian Sea
Cyclone frequency~80% of India's cyclones~20%
Sea Surface TemperatureWarmer; less upwellingCooler historically (upwelling off Somalia/Oman)
SalinityLower (river input — Ganga, Brahmaputra, Irrawaddy) → warmer top layerHigher salinity
Pre-monsoon seasonVery active (April–June)Less active historically
Post-monsoon seasonMost active Oct–DecLess active
IntensificationRapid deepening commonHistorically moderate

Arabian Sea — The Changing Picture

  • 2021 Nature study: Arabian Sea cyclone intensity has increased 40% since 1982 and is projected to increase further
  • Reason: Indian Ocean warming → AS SSTs rising faster than historical → more fuel for cyclones
  • Recent major AS cyclones: Biparjoy (2023) — ESCS that struck Gujarat (Mandvi); first major AS cyclone to hit Gujarat in decades

Seasonal Pattern

SeasonMonthsBasinReason
Pre-monsoonApril–JuneAS and BoBSSTs warm; no monsoon shear yet
MonsoonJuly–SeptemberSuppressedStrong wind shear prevents cyclone development
Post-monsoonOctober–DecemberBoB dominantSSTs warm after monsoon; low shear

Most destructive season: October–December (post-monsoon BoB) — strikes Odisha, Andhra Pradesh, Tamil Nadu coast


Major Cyclones Affecting India

CycloneYearBasinLandfall StateCategoryDeathsKey Notes
Bhola1970BoBBangladesh/WB~500,000Deadliest cyclone in recorded history
Odisha Supercyclone1999BoBOdisha (Paradip)SUCS~10,000Transformed India's DRR approach
Phailin2013BoBOdisha (Gopalpur)ESCS45Odisha evacuated 1 million — deaths reduced dramatically
HudHud2014BoBAP (Visakhapatnam)ESCS124₹21,908 crore damage; Visakhapatnam devastated
Fani2019BoBOdisha (Puri)ESCS641.2 million evacuated; Odisha model praised globally
Amphan2020BoBWB/OdishaSUCS128Strongest ever in BoB pre-landfall; Sundarbans devastated
Yaas2021BoBOdisha (Balasore)VSCS19Struck during COVID-19; coordinated evacuation
Tauktae2021ASGujaratESCS155Strongest AS cyclone in Gujarat since 1998
Biparjoy2023ASGujarat (Mandvi)ESCS4Very slow-moving; 9 days at sea; unprecedented
Michaung2023BoBAP/TNSCS26Caused extreme Chennai flooding
Remal2024BoBBangladesh/WBSCS~40Late May 2024; Sundarbans again
Dana2024BoBOdisha (Bhitarkanika)VSCS~30October 2024; Bhitarkanika mangroves

The Odisha Cyclone Preparedness Model

1999 to 2019: The Transformation

Parameter1999 Supercyclone2019 Fani (same intensity area)
Deaths~10,00064
Evacuated~150,0001.2 million
Warning24 hours7-day advance forecast
SheltersFew880+ multi-purpose cyclone shelters
CommunicationLimitedReal-time; SMS alerts; radio

Key Elements of Odisha's Model

  1. Early Warning: 7-day forecast; IMD provides 5-day track; 48-hr landfall prediction accuracy improved dramatically
  2. Mandatory evacuation: Zero tolerance for remaining in coastal areas (10 km from coast); legal backing
  3. Cyclone shelters: 880+ multi-purpose shelters on stilts (flood-proof); capacity for 1.5 million people
  4. Odisha Disaster Rapid Action Force (ODRAF): State-level rapid response; ahead of NDRF deployment
  5. Community radio: 24x7 alerts in local languages
  6. Women's SHG networks: Reach last-mile — critical for mobility-impaired, elderly
  7. Pre-positioned relief: Food, medicine, search-and-rescue boats pre-deployed before landfall

UPSC Quote: Fani (2019) — 1 in a million deaths (ratio of deaths to evacuated) — praised by UN and WHO as a global model of disaster preparedness.


Disaster Risk Reduction (DRR) — Institutional Framework

Constitutional Basis and DM Act 2005

FeatureDetail
Disaster Management Act2005 — primary legislation; triggered by 2001 Gujarat earthquake and 2004 tsunami
NDMANational Disaster Management Authority — PM as Chairman; Union Cabinet Ministers as members
SDMAState Disaster Management Authority — CM as Chairman
DDMADistrict Disaster Management Authority — Collector/DM as head
NDRFNational Disaster Response Force — 16 battalions; paramilitary forces on deputation; rapid deployment
SDRFState Disaster Response Fund — for immediate response by states
NDRFNational Disaster Response Fund — Union fund for large-scale disasters

Sendai Framework for Disaster Risk Reduction (2015–2030)

FeatureDetail
AdoptedUN World Conference on DRR; Sendai, Japan; March 2015
Period2015–2030 (successor to Hyogo Framework 2005–2015)
4 Priorities(1) Understanding disaster risk; (2) Strengthening DRR governance; (3) Investing in DRR for resilience; (4) Enhancing disaster preparedness
7 Global TargetsReduce: deaths, affected people, economic losses, critical infrastructure damage; Increase: national strategies, international cooperation, early warning access
Focus shiftFrom response (Hyogo) to prevention and risk reduction
India's roleActive participant; NDMP 2019 aligned with Sendai targets

CDRI — Coalition for Disaster Resilient Infrastructure

FeatureDetail
Founded byIndia — PM Modi announced at UNGA 2019; launched at COP26 Glasgow (2021)
Full nameCoalition for Disaster Resilient Infrastructure
SecretariatNew Delhi
Members40+ countries, 8 international organisations (as of 2024)
FocusMake new and existing infrastructure disaster and climate resilient
India's NITI AayogChairs CDRI Governing Council
SIDS InitiativeSpecial programme for Small Island Developing States — climate vulnerable nations

Flood Geography of India

Floods are India's most frequent and widespread disaster — affecting the Indo-Gangetic Plain, northeastern states, and coastal deltas every monsoon:

Most Flood-Prone Regions

RegionCauseStates
Bihar (Kosi basin)Himalayan rivers; changing channels; Nepal catchmentBihar
Assam (Brahmaputra)World's most flood-prone river valley; 3× annual floodsAssam
UP (Ganga-Ghaghra-Rapti)Monsoon surge; inadequate drainageUttar Pradesh
West Bengal (Damodar, Hooghly)DVC dams; upstream releaseWest Bengal
Coastal deltas (Krishna, Godavari, Mahanadi)Cyclone storm surge + river floodingAP, Odisha
Mumbai (urban)Choked stormwater drains + sea; 2005, 2017, 2024 eventsMaharashtra

Kosi — "Sorrow of Bihar"

  • Kosi has 120 major floods since 1953; changes course frequently (moved 110 km westward over 250 years)
  • 2008 Kosi breach: Most devastating in recent history — embankment breach in Nepal; 2.5 million displaced in Bihar
  • Kosi High Level Dam: Proposed — India-Nepal cooperation; long-pending
  • Kosi Barrage (Bhimnagar): Existing; regulates some flow; not enough

Flood Management Programme (FMP)

  • Central scheme; flood embankments, drainage channels, anti-erosion works
  • Target: Protect 40 million ha; only ~22 million ha protected so far

Earthquake Zones of India

India is divided into 4 Seismic Zones (II–V) by BIS (Bureau of Indian Standards) — IS 1893:2016:

ZoneIntensityStates/Regions
Zone V (Most severe; MSK IX+)Highest riskJ&K, HP (Kangra), Uttarakhand, entire NE India, Rann of Kutch, A&N Islands, North Bihar
Zone IV (MSK VIII)High riskDelhi NCR, parts of J&K, NW Himalayas, Sikkim, Indo-Gangetic plain, N AP
Zone III (MSK VII)ModerateMost of Kerala, Karnataka, Tamil Nadu, Maharashtra (except Kutch), Goa, UP, parts of Rajasthan
Zone II (MSK VI)Low riskParts of South India, Rajasthan desert, NW India (west Rajasthan)

Note: There is no Zone I in India's current seismic zonation.

Major earthquakes in India's history:

  • Bihar-Nepal (1934): M8.1; ~11,000 deaths
  • Latur (1993): M6.4; Deccan; 10,000 deaths; struck Zone III — showed risk even in lower zones
  • Jabalpur (1997): M6.0; similar lesson
  • Gujarat/Kutch (2001): M7.7; Bhuj; ~20,000 deaths; triggered DM Act 2005
  • Kashmir (2005): M7.6; ~80,000 deaths (including PoJK)
  • Sikkim (2011): M6.9; 111 deaths
  • Nepal (2015): M7.8 (Gorkha); 9,000 deaths; affected NE India

Key Facts for UPSC

  1. Tropical cyclone: Sustained winds ≥63 km/h over warm ocean; needs SST ≥26°C, Coriolis effect, low wind shear
  2. BoB cyclones: ~80% of India's total; Bay of Bengal warmer, less saline, less upwelling
  3. AS intensification: +40% intensity increase since 1982 (Nature 2021); Indian Ocean warming
  4. IMD categories: D → DD → CS → SCS → VSCS → ESCS → SUCS (7 levels)
  5. Bhola (1970): ~500,000 deaths — deadliest cyclone in history; Bangladesh/WB
  6. Odisha 1999 Supercyclone: ~10,000 deaths; triggered complete overhaul of India's DRR
  7. Fani (2019): ESCS; Odisha (Puri); 1.2 million evacuated; 64 deaths; 7-day warning; global model
  8. Amphan (2020): SUCS; strongest BoB cyclone pre-landfall; 128 deaths; Sundarbans devastated
  9. Odisha model: 880+ cyclone shelters; ODRAF; 7-day warning; mandatory evacuation
  10. DM Act 2005: NDMA (PM chairs), SDMA (CM chairs), DDMA (DM/Collector chairs)
  11. NDRF: 16 battalions; rapid deployment; paramilitary personnel on deputation
  12. Sendai Framework: 2015–2030; Sendai, Japan; 4 priorities; 7 global targets; successor to Hyogo
  13. CDRI: India-founded; announced UNGA 2019; launched COP26 2021; secretariat New Delhi; 40+ members
  14. Kosi — Sorrow of Bihar: 120 floods since 1953; course shifted 110 km westward over 250 years
  15. Seismic Zone V: Highest risk; J&K, Uttarakhand, NE India, Rann of Kutch, A&N Islands
  16. Bhuj earthquake (2001): M7.7; ~20,000 deaths; triggered DM Act 2005
  17. Latur (1993): M6.4; Zone III — proved even moderate zones can see high casualties
  18. Biparjoy (2023): ESCS; Gujarat (Mandvi); 9 days at sea; unprecedented slow-moving AS cyclone
Key Facts(18 of 18)
1 UPSC PYQ

UPSC Previously Asked

  • UPSC Quote: Fani (2019) — 1 in a million deaths (ratio of deaths to evacuated) — praised by UN and WHO as a global model of disaster preparedness.

A tropical cyclone is an organised rotating weather system over warm tropical oceans with sustained winds ≥63 km/h. The same system is called a 'cyclone' in the Indian Ocean, 'hurricane' in the Atlantic/Eastern Pacific, 'typhoon' in the Western Pacific, and 'willy-willy' in Australia.

Six conditions are required for tropical cyclone formation: Sea Surface Temperature (SST) ≥26–27°C to a depth of 60 m, atmospheric instability, Coriolis effect (minimum 5° from equator), low vertical wind shear, a pre-existing low-pressure disturbance, and high relative humidity in the middle troposphere.

The Bay of Bengal accounts for ~80% of India's tropical cyclones. Key reasons include lower salinity (from river inflow of Ganga, Brahmaputra, Irrawaddy), warmer SSTs due to reduced upwelling, and an enclosed geometry that sustains surface heat.

Arabian Sea cyclone intensity has increased by 40% since 1982 (Nature Climate Change, 2021), driven by warming Indian Ocean sea surface temperatures. Historically less active, the Arabian Sea is producing increasingly powerful cyclones during the pre-monsoon season.

Cyclone Bhola (1970) struck Bangladesh and West Bengal and killed ~500,000 people — making it the deadliest tropical cyclone in recorded history. The 1999 Odisha Supercyclone killed ~10,000 people and completely transformed India's disaster risk reduction approach.

Cyclone Fani (2019) — an Extremely Severe Cyclonic Storm — made landfall at Puri, Odisha. Despite its intensity, only 64 people died after 1.2 million people were evacuated with 7-day advance warning. This 'one in a million' deaths-to-evacuated ratio was praised by the UN as a global model.

Cyclone Amphan (2020) was the strongest Bay of Bengal cyclone ever recorded before landfall — classified as a Super Cyclonic Storm. It made landfall on the West Bengal/Odisha border, caused ₹1 lakh crore in damage, and devastated the Sundarbans.

Cyclone Biparjoy (June 2023) was an Extremely Severe Cyclonic Storm that spent 9 days at sea — an unprecedented slow-moving Arabian Sea cyclone — before making landfall near Mandvi (Jakhau area), Gujarat. It is the strongest pre-monsoon Arabian Sea cyclone on record.

Odisha's cyclone preparedness model transformed outcomes between 1999 and 2019: deaths fell from ~10,000 to 64 (Fani), while evacuations rose from 150,000 to 1.2 million. The model's key elements are 880+ multi-purpose cyclone shelters, ODRAF (Odisha Disaster Rapid Action Force), 7-day advance forecasting, and community radio alerts.

The IMD classifies tropical cyclones in 7 categories by wind speed: Depression (D), Deep Depression (DD), Cyclonic Storm (CS), Severe Cyclonic Storm (SCS), Very Severe Cyclonic Storm (VSCS), Extremely Severe Cyclonic Storm (ESCS), and Super Cyclonic Storm (SUCS, ≥222 km/h).

The Disaster Management Act, 2005 — triggered by the 2001 Bhuj earthquake and the 2004 Indian Ocean Tsunami — established a three-tier DM structure: NDMA (national level, chaired by the PM), SDMA (state level, chaired by CM), and DDMA (district level, chaired by the District Collector/DM).

The National Disaster Response Force (NDRF) has 16 battalions drawn from paramilitary forces (BSF, CRPF, ITBP, CISF, SSB). It specialises in urban search and rescue (USAR), flood rescue, and mountain rescue, and is pre-positioned before cyclones and floods.

The Sendai Framework for Disaster Risk Reduction (2015–2030) was adopted at Sendai, Japan in March 2015 and is the successor to the Hyogo Framework (2005–2015). It has 4 priorities and 7 global targets, and marks a shift from disaster response toward prevention and risk reduction.

The Coalition for Disaster Resilient Infrastructure (CDRI) was founded by India — announced by PM Modi at UNGA 2019 and officially launched at COP26 Glasgow (2021). Its secretariat is in New Delhi, it has 40+ member countries and 8 international organisations, and focuses on making infrastructure climate and disaster resilient.

The Kosi River (Bihar) is called the 'Sorrow of Bihar.' It has experienced 120 major floods since 1953 and has shifted its course ~110 km westward over 250 years through channel avulsions. The catastrophic 2008 breach in Nepal displaced 2.5 million people in Bihar.

India's seismic zonation (IS 1893:2016) divides the country into four zones (II to V) — there is no Zone I. Zone V (highest risk) covers all of northeastern India, J&K/Ladakh (parts), Uttarakhand foothills, Rann of Kutch, north Bihar, and the Andaman & Nicobar Islands.

The Bhuj earthquake (2001, M7.7) killed ~20,000 people, destroyed 400,000+ buildings in Kutch, Gujarat, and directly triggered the enactment of the Disaster Management Act, 2005. The Latur earthquake (1993, M6.2–6.4) killed ~10,000 in Maharashtra's Zone III — demonstrating that moderate seismic zones can experience catastrophic casualties.

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