Cyclone Amphan: The Super Storm That Roared!

Examining the formation, unprecedented intensity, and devastating socio-economic impacts of Super Cyclonic Storm Amphan in May 2020 across the Bay of Bengal region.

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Post Cyclone Amphan situation of Deshbandhu park in Kolkata 03

Post Cyclone Amphan situation of Deshbandhu park in Kolkata 03

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Cyclone Amphan: Narendrapur
Cyclone Amphan (2020) chart
Cyclone Amphan: Narendrapur
Post Cyclone Amphan situation of house of Bhupendra Bose in Kolkata 01
Post Cyclone Amphan situation of Shyambazar in Kolkata 44
Cyclone Amphan (2020) map
Cyclone Amphan: Narendrapur
Cyclone Amphan: Narendrapur
Cyclone Amphan: Narendrapur
Post Cyclone Amphan situation of Deshbandhu park in Kolkata 18
Post Cyclone Amphan situation of Dilarjung road in Kolkata 01

Genesis and Rapid Intensification Over Anomalously Warm Waters

Super Cyclonic Storm Amphan, the first tropical cyclone of the 2020 North Indian Ocean season, emerged from a low-pressure area east of Sri Lanka on May 13, 2020. Its development was significantly influenced by exceptionally warm sea surface temperatures in the Bay of Bengal, which provided abundant heat energy for intensification. The Joint Typhoon Warning Center (JTWC) and the India Meteorological Department (IMD) closely monitored its rapid ascent.

Amphan underwent explosive intensification, transitioning from a severe cyclonic storm to an extremely severe one in just 12 hours on May 17th. This rapid intensification is a critical factor in the destructive potential of modern cyclones, often leaving communities with less time for preparation and evacuation. The storm's trajectory was initially northeastward, a path that took it over waters conducive to extreme strengthening.

Peak Intensity, Eyewall Replacement, and Landfall Dynamics

Amphan reached its zenith on May 18th, boasting 3-minute sustained winds of 240 km/h (150 mph) and 1-minute sustained winds of 270 km/h (170 mph), with a remarkably low central barometric pressure of 920 mbar. This placed it firmly in the 'super cyclonic storm' category. Shortly after achieving peak intensity, the storm began an eyewall replacement cycle, a natural process where an outer eyewall forms and contracts, potentially leading to weakening.

However, factors like dry air intrusion and wind shear disrupted this cycle, contributing to a gradual weakening as Amphan paralleled the Indian coastline. Despite this weakening, its landfall in West Bengal on May 20th, with estimated 1-minute sustained winds of 175 km/h (110 mph), was still catastrophic, underscoring the immense energy retained by the storm.

Unprecedented Economic and Environmental Devastation

The impact of Cyclone Amphan was profound and far-reaching. It inflicted over US$15 billion in damages, establishing a new record for the costliest cyclone in the North Indian Ocean, surpassing Cyclone Nargis. This economic toll reflects the extensive destruction of infrastructure, homes, and livelihoods across affected regions.

West Bengal, including major urban centers like Kolkata, and the coastal districts of Odisha bore the brunt of the storm's fury. In Bangladesh, the cyclone's reach extended to northern regions like Rajshahi and Rangpur, causing significant damage to agriculture, notably impacting mango production. The storm's passage through the Ganges Delta, a region characterized by its low elevation and high population density, amplified its destructive consequences, leading to widespread displacement and humanitarian challenges.

Geopolitical and Climate Change Context

Amphan's occurrence within the context of the 2020 cyclone season, and its extreme intensity, raises questions about the influence of climate change on tropical cyclones. Warmer ocean temperatures are a known factor in fueling more powerful storms. The storm's name, 'Amphan,' meaning 'sky' in Thai, highlights the collaborative naming conventions for cyclones in the region.

Its status as the strongest cyclone to hit the Ganges Delta and the most powerful to strike India since 1999 underscores the increasing threat posed by extreme weather events. The cyclone's trajectory and intensity serve as a critical case study for disaster preparedness, climate adaptation strategies, and the urgent need for global action on climate change mitigation.

See also

Frequently Asked Questions

What was Cyclone Amphan?+
Cyclone Amphan was a very strong storm that formed in the Bay of Bengal in May 2020. It was the first big storm of that year in the North Indian Ocean.
How strong was Cyclone Amphan?+
At its peak, the storm had winds up to 270 km/h (170 mph) and a very low pressure of 920 mbar, making it a super cyclonic storm.
Where did Cyclone Amphan hit?+
It made landfall in West Bengal, India, and also affected parts of Bangladesh like Rajshahi and Rangpur.
Why was Cyclone Amphan so powerful?+
The water in the Bay of Bengal was very warm, giving the storm extra heat and energy, and it grew very fast in just 12 hours.
What happened to people and homes during Cyclone Amphan?+
The storm caused huge damage, costing more than US$15 billion, and many homes, farms, and cities like Kolkata were badly affected, leaving many people displaced.
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