Minimalist IAS
2024 GS Paper I

UPSC CSE (Main) 2024 · GS Paper I · Question 4

What is sea surface temperature rise? How does it affect the formation of tropical cyclones?

Syllabus line: Geophysical phenomena & changing features — “Important Geophysical phenomena such as earthquakes, Tsunami, Volcanic activity, cyclone etc., geographical features and their location-changes in critical geographical features (including water-bodies and ice-caps) and in flora and fauna and the effects of such changes.”

GS Paper I 2024 · Q4

10 marks · 150 words Geophysical phenomena & changing features

What is sea surface temperature rise? How does it affect the formation of tropical cyclones?

Approach · directive: “what / how”

What it asks · Define the warming of the ocean's upper layer and explain the physical link between warmer seas and the genesis, intensity and frequency of tropical cyclones.

The question has 2 parts — answer each

  1. Define sea surface temperature rise and what drives it
  2. Explain how SST rise affects the formation of tropical cyclones: energy supply, intensity, frequency and location, and the other conditions still required

Open with · Tropical cyclones are heat engines fuelled by warm ocean water — sea surface temperature of roughly 26–27°C and above is a classic precondition for their formation.

Cover

  • Meaning: sea surface temperature (SST) is the temperature of the ocean's top layer; its rise reflects greenhouse warming, marine heatwaves and ENSO/IOD phases.
  • Energy supply: warmer water raises evaporation; latent heat released in rising air strengthens convection and deepens the low-pressure centre.
  • Intensity: high SST with deep ocean heat content allows rapid intensification — Ockhi (2017) and Tauktae (2021) jumped categories quickly.
  • Frequency and location: a warmer Arabian Sea now supports more and longer-lived cyclones; seasons may lengthen.
  • Other conditions still needed: Coriolis force away from the equator, low vertical wind shear, a pre-existing disturbance and upper-level divergence.
  • Impacts: heavier rainfall, stronger winds and higher storm surge, made worse by sea-level rise along low coasts.

Close with · Warmer seas are loading cyclones with more energy; forecasting, coastal zoning, shelters and mangrove buffers must keep pace.

Add value (verified)

  • Ministry of Earth Sciences told Parliament (2021) that cyclonic storm formation shows a decreasing trend over the Bay of Bengal but an increasing trend over the Arabian Sea. Study on Cyclones — PIB, Ministry of Earth Sciences, 15 March 2021 ↗“Studies show a decreasing trend in the frequency of formation of Cyclonic Storms over the Bay of Bengal and an increasing trend over the Arabian Sea”

Question: UPSC's CS (Main) 2024, GS Paper I — paper ↗. Approach: Minimalist IAS, checked 30 Sept 2026 (how we verify) — UPSC publishes no model answers. ·

Model answer · 228 words (UPSC limit 150) · Minimalist IAS

Tropical cyclones are heat engines fuelled by warm ocean water; a sea surface temperature of about 26–27°C through a deep layer is a precondition for their formation.

What SST rise means

  • Sea surface temperature is the temperature of the ocean's top layer.
  • Its rise reflects greenhouse warming, marine heatwaves and warm phases of ENSO and the Indian Ocean Dipole, and it deepens the ocean's heat content.

How it affects cyclone formation

  • More fuel: warmer water raises evaporation; latent heat released as vapour condenses in rising air deepens the low-pressure core and drives the vortex.
  • Wider window: the threshold is met over larger areas and for longer, extending the season and zone of genesis.
  • Intensity: deep warm layers stop storms from stirring up cold water, allowing rapid intensification — Ockhi (2017), Amphan (2020) and Tauktae (2021) jumped categories within a day.
  • Location: a warming Arabian Sea breeds more and longer-lived cyclones (Biparjoy, 2023); in 2021 the Ministry of Earth Sciences reported a rising trend there and a falling one over the Bay of Bengal.
  • Not sufficient alone: genesis still needs Coriolis force, low vertical wind shear, a pre-existing disturbance and upper-level divergence, so frequency responds unevenly across basins.
  • Impacts: heavier rain, stronger winds and higher storm surge, compounded by sea-level rise.

Warmer seas are loading cyclones with more energy; forecasting, coastal zoning, shelters and mangrove buffers must keep pace.

Written by Minimalist IAS from facts checked at source (how we verify) — a little fuller than exam length, so every part of the question is covered; in the hall, keep the structure and trim the detail. UPSC publishes no model answers: compare your structure and coverage with this, then write your own.

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