UPSC Mains
GS Paper I & III
Geography & Disaster Management
Cyclone Arnab: How El Niño Shaped Its Path and Intensity
Cyclone Arnab made landfall on 28 October on the Andhra Pradesh and Yanam coasts as a very severe cyclonic storm, and an explainer links its fast intensification and path to this year’s El Niño
LANDFALL
28 October
NIÑO 3.4 ANOMALY
2 to 2.8°C above normal
EVACUATED
1.8 lakh people
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Why in News
Cyclone Arnab made landfall on 28 October on the Andhra Pradesh and Yanam coasts as a very severe cyclonic storm, with flash flood warnings for 13 districts. An explainer links its fast intensification and its path to this year’s El Niño.
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How did El Niño change the cyclone’s route?
El Niño shifts where Bay of Bengal cyclones form and where they strike.
- Usual pattern: Odisha and West Bengal are the coasts most prone to Bay of Bengal cyclones.
- In El Niño years: Cyclones tend to form at lower latitudes, so they are more likely to move towards Andhra Pradesh and Tamil Nadu, as the IMD chief had explained. Cyclone Hudhud (2014), another El Niño year, hit the Andhra coast.
- Post-monsoon winds: After the monsoon withdraws in mid-October, the monsoon trough moves south. A warmer ocean under El Niño also changes wind and air pressure near the equator.
Note: In an El Niño year, the risk moves south along the east coast.
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Why did Arnab intensify so fast?
- Warm ocean: In July to September 2026, the sea surface temperature in the Niño 3.4 region was 2 to 2.8°C above normal. Ocean temperatures of 26°C or more at 50 to 100 metres depth help cyclones form, and Arnab reached its peak intensity in a single day.
- Other factors: Intensification also depends on wind shear, convection, upper ocean circulation and air-sea interaction.
- Speed: Cyclones formed in these conditions also move faster, as Arnab did.
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Why did Arnab stay strong after landfall?
- Normal pattern: A cyclone usually loses strength once it moves over land.
- Arnab: It kept its strength for at least six hours and stayed nearly stationary near Narsapur and Yanam from 4 am, which slowed the landfall process. Landfall normally takes up to six hours or more, depending on the cyclone’s speed and size.
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Challenges
- Forecasting rapid intensification: Arnab strengthened and moved faster than forecast.
- Inland flooding: Remnants of the cyclone can bring heavy rain far from the coast, as in Telangana, Bihar and east UP.
- Shifting risk: Andhra Pradesh and Tamil Nadu need to prepare more in El Niño years.
- Coastal geography: The Bay of Bengal is funnel-shaped, landlocked on three sides and shallow near the coast, so it is prone to storm surges.
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Prelims Pointers
- Arnab: Named by Bangladesh. Next names are Murasu (India, Tamil for drum) & Akvan (Iran).
- Naming: The WMO/ESCAP Panel on Tropical Cyclones (13 members) began naming in September 2004. A list of 169 names was adopted in April 2020.
- Landfall: When the cyclone’s eye crosses the coast. Yanam is a Puducherry enclave on the Andhra coast.
- Formation needs: Sea surface of about 26 to 27°C or more, low wind shear, moist air, the Coriolis force and an existing disturbance.
- Season: October to December is the main cyclone season in the Bay of Bengal.
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Way Forward
Better forecasts
Improve forecasts of rapid intensification and of stalling after landfall, using ocean and high-resolution data.
Early evacuation
Use impact-based warnings and move people earlier, as in the evacuation of 1.8 lakh.
Resilient infrastructure
Build cyclone shelters, power and communication networks that withstand strong winds.
Inland preparedness
Prepare inland states for flood risk from remnants of coastal cyclones.
Conclusion: Arnab showed how El Niño can move cyclone risk to different coasts and speed up a storm. Preparedness must follow the changing risk and not the usual pattern.
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Source: The Indian Express

