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Cyclone Fani

North Indian Ocean cyclone in 2019

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Through Bangladesh

Prior to Fani's landfall, authorities in India and Bangladesh moved at least a million people each from areas within Fani's projected path onto higher ground and into cyclone shelters, which is thought to have reduced the death toll. Fani killed at least 81 people in eastern India and Bangladesh and caused about US$8.1 billion worth of damage in both India and Bangladesh, mostly in Odisha, in India.

Meteorological history

On 26 April, the India Meteorological Department (IMD) began tracking a depression located to the west of Sumatra, designating it as BOB 02, meaning the second depression of 2019 formed in the Bay of Bengal, the first being Tropical Storm Pabuk earlier that year. Later that day, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert on the system. Afterward, the storm slowly coalesced while moving northward, and was upgraded to a deep depression at 03:00 UTC on 27 April. At the same time, the JTWC began warning on the system, designating it 01B. Six hours later, the IMD upgraded the system to a cyclonic storm and gave it the name Fani.

The system continued to intensify until 18:00 UTC on 27 April, after which it stagnated for over a day while continuing to move northwest. On 29 April, Fani resumed strengthening around 12:00 UTC, with the IMD upgrading it to a severe cyclonic storm. At that time, Fani began a period of rapid intensification as it was located within a very favorable environment with sea surface temperatures of 30–31 °C (86–88 °F) and low vertical wind shear. As a result, the JTWC upgraded Fani to a Category 1-equivalent cyclone late on 29 April. Around 00:00 UTC on 30 April, Fani was upgraded to a very severe cyclonic storm by the IMD. The organization of the system continued to improve, with tight spiral banding wrapping into a formative eye feature, resulting in Fani being upgraded to an extremely severe cyclonic storm by the IMD around 12:00 UTC, while the JTWC upgraded the storm to a Category 3-equivalent cyclone hours later. On 2 May, the central dense overcast became more symmetrical and the eye more distinct, and Fani was upgraded to a Category 4-equivalent cyclone by the JTWC at 06:00 UTC. Shortly after, Fani started another period of rapid intensification, attaining 1-minute sustained winds of 280 km/h (175 mph) according to the JTWC. It became the strongest pre-monsoon cyclone in the Bay of Bengal since 1991. Operationally, the JTWC classified the system as a high-end Category 4-equivalent tropical cyclone with 1-minute sustained winds of 250 km/h (155 mph), but raised their estimate in post-season re-analysis.

Fani quickly weakened after peak intensity. In the morning of 3 May, Fani made landfall near Puri, Odisha as an extremely severe cyclonic storm with 3-minute sustained winds of 185 km/h (115 mph) and 1-minute sustained winds of 230 km/h (145 mph) according to IBTrACS, a dataset of best tracks. This made Fani the most intense storm to make landfall in India's Odisha state since the 1999 Odisha cyclone. Land interaction quickly degraded Fani's convective structure and it weakened to a Category 1-equivalent tropical cyclone soon after landfall. Fani continued to weaken after landfall, weakening to a cyclonic storm later that day, before passing just north of Kolkata. On 4 May, Fani weakened to a deep depression and moved into Bangladesh, before degenerating into a well-marked low later on the same day. Fani's remnant low dissipated over Myanmar the next day.

Relation to climate change

Fani underwent rapid intensification as it tracked northward over the Bay of Bengal, where local sea surface temperatures were 2.5 °C (4.5 °F) above normal. A convection‑permitting attribution study with WRF‑Chem found that removing post‑1990 warming trends in both the atmosphere and ocean reduced Fani's five‑day precipitation totals by around 51%, with tropospheric warming contributing roughly two‑thirds of this reduction and sea surface warming roughly one‑third.

Fani has been part of a recent trend of cyclones forming at unusual times of year. Between 1891 and 2019, Fani is one of only 15 severe cyclones to form in April, with only one other storm also crossing the Indian mainland.

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