The 2020 North Indian Ocean cyclone season was at that time, the costliest North Indian Ocean cyclone season on record, until it was surpassed 5 years later, mostly due to the devastating Cyclone Amphan. It was an above average season featuring 5 cyclonic storms. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and November, with peaks in late April to May and October to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. In 2020, the cyclone season began on May 16 with the designation of Depression BOB 01 in the Bay of Bengal, which later became Amphan. Cyclone Amphan was the strongest storm in the Bay of Bengal in 21 years and broke Nargis of 2008's record as the costliest storm in the North Indian Ocean. The season concluded with the dissipation of Cyclone Burevi on December 5. Overall, the season was slightly above average, seeing the development of five cyclonic storms.
The scope of the season is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula. There are two main seas in the North Indian Ocean – the Arabian Sea to the west of the Indian subcontinent, abbreviated ARB by the India Meteorological Department (IMD); and the Bay of Bengal to the east, abbreviated BOB by the IMD.
The official Regional Specialized Meteorological Centre in the basin is the India Meteorological Department (IMD), while the United States's Joint Typhoon Warning Center (JTWC) releases unofficial advisories. On average, three to four cyclonic storms form in this basin every season.
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Season summary
The season began on May 16 with the designation of Depression BOB 01 in the Bay of Bengal, which later became Cyclone Amphan, the strongest storm in the Bay of Bengal recorded since the 1999 Odisha cyclone and breaking the record of Cyclone Nargis of 2008 as the costliest storm ever recorded in the basin. Two more cyclones formed in the Arabian Sea, ARB 01, affecting Yemen and Oman, and Cyclone Nisarga, which made landfall in Maharashtra. After a four-month pause of activity, BOB 02 formed, causing 98 fatalities. Its remnants formed ARB 03. It was a weak storm. After 2 days, BOB 03 formed, impacting and affecting West Bengal, Bangladesh and Northeast India. It was also a weak storm, lasting for 2 days. After its break, Cyclone Gati formed, leaving 8 confirmed, 30 missing as of today, on Somalia and Yemen, where the cyclone took place. On November 23, a depression formed in the Bay of Bengal, and it strengthened into Very Severe Cyclonic Storm Nivar, two days later. It made landfall between Puducherry and Chennai close to Mahabalipuram in the midnight of November 25. It weakened into a well marked low pressure in the early hours of November 27. On November 28, a low pressure formed off the coast of Tamil Nadu, it gradually intensified into a depression, BOB 05. It later intensified into a deep depression and then into a cyclonic storm, named Cyclone Burevi. It made landfall on Sri Lanka as a weak cyclonic storm before it degenerated to an area of low pressure.
Systems Super Cyclonic Storm Amphan
At 00:00 UTC on May 16, a depression formed in the southeast Bay of Bengal and was identified as BOB 01. Six hours later, the India Meteorological Department (IMD) upgraded the system to a deep depression. The system began bringing torrential rainfall to Sri Lanka and Southern India. Around 15:00 UTC, the system further developed into Cyclonic Storm Amphan. That morning, landslide and flooding warnings were hoisted for parts of eastern Sri Lanka and the Indian state of Kerala were given expectations of torrential rainfall in the coming days. By 09:00 UTC on May 17, Amphan had intensified into a very severe cyclonic storm. Within 12 hours, the storm had developed an eye and started to rapidly intensify, becoming an extremely severe cyclonic storm. According to the JTWC, it explosively intensified from a Category 1-equivalent cyclone to a Category 4-equivalent cyclone in just 6 hours. The following morning around 10:30 UTC, the IMD upgraded Amphan to a super cyclonic storm with 3-minute sustained winds of and a minimum pressure of . This marked the second year in a row featuring a super cyclonic storm, the previous year seeing Kyarr in the Arabian Sea. On May 20, at approximately 17:30 IST, the cyclone made landfall near Bakkhali, West Bengal after weakening subsequently. It rapidly weakened once inland, and dissipated on the next day. It left behind a trail of catastrophic damage, and was later confirmed to be the costliest storm ever recorded in the basin, until Cyclone Senyar surpassed it in November 2025.
Depression ARB 01
A depression formed overland near Salalah, Oman on May 29.
The Public Authority for Civil Aviation (PACA) in Oman advised residents to exercise caution and not to venture to low-lying areas or sea. The Supreme Committee asked people to remain at home in non-emergency circumstances. The hospital in Sadah was evacuated as the depression intensified. Over of rain fell in Dhofar Governorate on May 29; some areas received the equivalent of 2 years of rainfall. The highest precipitation total was measured in Mirbat, where of rain fell. 2 days of heavy rainfall, accumulating to , caused floods in Salalah. Operations at the port of Salalah were interrupted by the tropical depression. Residents in central Salalah experienced disruptions to power and water services. Military police were dispatched to clear roads and airlift people marooned by the floods. Engineering teams from the Ministry of Defence were deployed to restore utilities and render air where necessary. 2 people were found dead in a wadi due to flash floods, while another person died and three were injured when a building collapsed. More than 50 people were rescued from floods.
Severe Cyclonic Storm Nisarga
During May 31, an area of low pressure developed over the south-eastern Arabian Sea and remained as a well marked low-pressure area over the same region until the evening. It strengthened into a depression over the east-central and south-east Arabian Sea in the early morning of June 1 when it was centered about 340 km south-west of Goa, 630 km south-southwest of Mumbai and 850 km south-southwest of Gujarat. It gave nearly 400 mm of extremely heavy rain at Kavaratti, Lakshadweep. On June 2, around noon, the prevailing deep depression intensified into a cyclonic storm thereby receiving the name Nisarga. Nisarga intensified into a severe cyclonic storm before making landfall near the coastal town of Alibag in Maharashtra at 12:30 (IST) on June 3. At the time, the system was at peak intensity with 3-minute sustained winds of and a central pressure of . The cyclone subsequently weakened into a deep depression by June 4.
Deep Depression BOB 02
After 3 months of inactivity, on October 11, a depression developed over the west-central Bay of Bengal, though the system was originally observed near the Spratly Islands over the South China Sea on October 6. It continued to move westwards, making landfall in the Khánh Hòa province and further weakened into a low pressure cell while crossing the Indochina Peninsula and re-emerged in the Andaman Sea on October 9. It intensified into a well-marked low-pressure area and then into a depression over the Bay of Bengal on October 10. It further intensified into a deep depression on October 12, remaining practically stationary over the same region. After that, BOB 02 moved west-northwestwards and made landfall in Andhra Pradesh near Kakinada in the early hours of October 13 and weakened again into a depression. The system weakened into a well-marked low-pressure area in south-central Maharashtra on the evening of October 14. Though the system's lower-level circulation was partially exposed due to high vertical wind shear and continuous land interaction, the JTWC re-issued a tropical cyclone advisory on October 15. The IMD also forecasted BOB 02 to reintensify in the Arabian Sea. The low-pressure area intensified into Depression ARB 03 on the early hours of October 17.
Due to BOB 02, Yanam (Puducherry), Andhra Pradesh, Telangana, Kerala, Maharashtra, and coastal Karnataka experienced heavy rain on October 12 and 13, with Hyderabad experiencing 32 cm of record-breaking torrential rain, creating flash floods in the city by October 13. At least 50 people died in different parts of Telangana (of which at least 19 were in the capital city of Hyderabad), 10 in Andhra Pradesh, and 38 in Maharashtra. Extreme crop loss in north Karnataka, Andhra Pradesh and Telangana occurred due to the system. The Telangana CM estimated damage costs to be ₹1,305 crore (US$682 million).
The system delayed the withdrawal of the southwest monsoon season by almost a week, a delay compounded by the formation of Depression ARB 03 and Depression BOB 03.
Depression ARB 03
On October 17, the remnants of Deep Depression BOB 02 intensified into a depression in the East Central Arabian Sea. Moving westwards, the system dissipated into a well marked low pressure on the morning of October 19 over the West Central Arabian Sea due to unfavorable atmospheric conditions.
Fishermen were advised not to go out to sea due to very rough sea conditions. Heavy rainfall occurred off the coast of Mumbai and its surroundings due to the system. No warnings were issued by IMD as no landfall occurred in the Arabian Peninsula.
Monsoon withdrawal was delayed in Maharashtra by a week due to ARB 03.
Depression BOB 03
On October 20, a low pressure formed over Central Bay of Bengal. The system then became more well-marked on October 21 over West Central Bay of Bengal. It further intensified into depression over northwest Bay of Bengal and adjoining Odisha Coast. The system crossed West Bengal's North 24 Parganas and South 24 Parganas and moved over the adjoining Bangladeshi coast on the noon of October 23 with the maximum wind speed of . The system weakened into a well marked low-pressure area, 50 km north-northwest of Dhaka on the morning of October 24.
Very Severe Cyclonic Storm Gati
On November 17, the India Meteorological Department (IMD) noted the potential for tropical cyclogenesis over the central Arabian Sea in association with an area of low pressure near the Maldives. Convective activity was enhanced by the Madden–Julian oscillation while sea surface temperatures of and low wind shear favored additional development. By November 18, a weak low-level circulation developed about east-southeast of Socotra. Organization thereafter was stymied as it became embedded within a monsoon trough. Two additional circulations developed to the east and west of the original low; however, the original low steadily became the dominant system by absorbing the previous two circulations. On November 21, two scatterometer passes revealed a single, well-defined low with gale-force winds underneath an area of flaring convection. At 18:00 UTC, the IMD classified the system as Depression ARB 04 about east-southeast of Socotra. Similarly, the Joint Typhoon Warning Center (JTWC) initiated advisories on the system as Tropical Cyclone 03A. Steered west by a subtropical ridge to the north, little intensification was expected before the cyclone's forecast landfall in Somalia.