North Indian Ocean tropical cyclone

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File:North Indian cyclone tracks 1970-2005.jpg
Cumulative track map of all North Indian Ocean cyclones from 1970 to 2005

In the Indian Ocean north of the equator, tropical cyclones can form throughout the year on either side of the Indian subcontinent, although most frequently between April and June, and between October and December.

The North Indian Ocean is the least active official basin, contributing only seven percent of the world's tropical cyclones. However the basin has produced some of the deadliest cyclones in the world, since they strike over very densely populated areas.[1] The Regional Specialized Meteorological Centre (RSMC) is the India Meteorological Department (IMD) and it is responsible to monitor the basin, issues warning and name the storms.[2]

Sub-basins

File:Luban and Titli 2018-10-10 0745Z–0926Z.jpg
Very severe cyclonic storms Luban (left) and Titli (right) over the Arabian Sea and the Bay of Bengal in October 2018

The basin is divided into two sub-basins Template:Snd the Bay of Bengal and the Arabian Sea.[3]

The Bay of Bengal, located in the northeast of the Indian Ocean. The basin is abbreviated BOB by the India Meteorological Department (IMD).[4] The United States's Joint Typhoon Warning Center unofficially designates as B to classify storms formed in the Bay of Bengal.[5] The Bay of Bengal's coast is shared among India, Bangladesh, Myanmar, Sri Lanka and western part of Thailand.[6] This sub-basin is the most active and produces some of the deadliest cyclones of all time.[7] The most intense cyclone in the bay was the 1999 Odisha cyclone.[8]

The Arabian Sea is a sea located in the northwest of the Indian Ocean. Tropical cyclones in the basin are abbreviated ARB by the India Meteorological Department (IMD).[4] The United States's Joint Typhoon Warning Center unofficially designates as A to classify storms formed in the Arabian Sea.[9] The Arabian Sea's coast is shared among Pakistan, India, Yemen, Oman, UAE, Iran, Sri Lanka, Maldives and Somalia.[10] Monsoons are characteristic of the Arabian Sea and responsible for the yearly cycling of its waters. In summer, strong winds blow from the southwest to the northeast, bringing rain to the Indian subcontinent. Cyclones are less frequent in the Arabian Sea, but the basin can produce strong tropical cyclones.[10] Cyclone Gonu was the strongest and the costliest recorded tropical cyclone in the basin.[11]

History of the basin

The systematic scientific studies of tropical systems in the Bay of Bengal and Arabian Sea was started during the 19th century by Henry Piddington.[12] Piddington utilised meteorological logs of vessels that navigated the seas and published a series of memoirs, in the Journal of the Asiatic Society of Bengal between 1839 and 1858.[12] These memoirs gave accounts and tracks of individual storms in the Bay of Bengal and the Arabian Sea.[12]

During the 2004 post monsoon season the IMD started to name tropical cyclones within the basin, with the first one named Cyclone Onil during September 2004.[13] During 2015 a modification to the intensity scale took place, with the IMD and WMO calling a system with 3-minute maximum sustained wind speeds between Script error: No such module "convert". and Script error: No such module "convert". an extremely severe cyclonic storm.[14]

A study analysing the spring season of tropical cyclones in the Bay of Bengal found increases in both pre-monsoon precipitation and tropical cyclone intensity as a result of enhanced large-scale monsoon circulation after 1979. The deepened monsoon trough in the Bay of Bengal not only affects cyclone frequency and timing, but also acts to direct more cyclones towards Myanmar. Increased anthropogenic aerosols likely contributed to such a regional climate change.[15]

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Climatology

Formation and frequency

On average only five to six tropical cyclones form in the basin each year. Tropical cyclones form in the months of March to June and October to December, with peaks at May and November. Most of these storms form in the Bay of Bengal: either in the southeastern Bay of Bengal, in the Andaman Sea, or as a remnant of a typhoon from the South China Sea, and a few in the Arabian Sea.[8] High sea surface temperatures and humidity makes the bays more favourable to tropical cyclone development.[16] There are many tropical cyclones in the West Pacific; this may be another reason for increasedScript error: No such module "Unsubst". tropical cyclogenesis in the Bay, as it shares a fair portion of the increased quota of ACE. Meanwhile, the storms in the Arabian Sea mostly form over south-eastern part of the Arabian Sea or a remnant of a tropical cyclone from the Bay of Bengal, however the frequency of cyclogenesis in the Arabian Sea is generally less, due to cooler sea surface temperature and high wind shear.[8] However a strong positive Indian Ocean Dipole may cause an increase of tropical cyclogenesis than usualScript error: No such module "Unsubst". which was seen in the 2019 season.[17] Very few tropical cyclones develop in the months of June to September (Monsoon months) because of high vertical wind shear. These storms form in the Bay of Bengal and peak as depressions or deep depressions before making landfall in Odisha or West Bengal. Another reason is the low life span in the seaScript error: No such module "Unsubst". which also avoids the intensification of these low-pressure systems.[8]

Movement

Most of the storms move in a north-westerly direction and starts curving either towards southwest or northeast. There's a higher frequency of recurving towards northeast rather going southwest. In the Arabian Sea these storms mostly move in north-westerly direction targeting the Arabian Peninsula, however in some case these storm moves north-eastwards after crossing the 15°N latitude and strikes the Gujarati coast. In the Bay of Bengal, storms generally moves north-westwards until reaching the east coast and then moves north-eastwards.[18]

Intensification

Intensification probability is maximum in the months of April, May and November in case of a depression becoming a cyclonic storm and severe cyclonic storm. More than half of the depressions intensify into a storm and a quarter intensify into a cyclone in these months.[19]

Landfall

In the Arabian Sea, most storms dissipate offshore without making landfall, but a significant number of tropical cyclones also impact the west coast, particularly the states of Gujarat and Maharashtra. The remaining 11 percent makes landfall in either the Arabian Peninsula, Horn of Africa or Pakistan.[20] In rare cases, some storms make landfall in Iran, like Cyclone Gonu did in 2007.[21] Other than Gonu, two storms: Cyclone Yemyin and Kyarr made some or major impact in Iran.[22][23]

In the Bay of Bengal, most of the storms strikes either the Indian states of Odisha or West Bengal and a significant number of storms hit the states of Andhra Pradesh and Tamil Nadu. 30 percent of the cyclones strike the countries of Bangladesh, Sri Lanka and Myanmar while the remaining 13 percent just dissipates off shore without making landfall.[20]

Climate change

Script error: No such module "Labelled list hatnote". After a series of devastating cyclones in 2018, rising number of cyclones in the Arabian Sea in 2019 and a rising trend of rapid intensification in 2020 and 2021, many climatologists agree that climate change have caused these activities. On average, five cyclonic storms occur every year in the Arabian Sea. However, in 2019 eight cyclonic storms formed, becoming the record highest number of tropical cyclones in the sub-basin, which was tied with the 1902 season.[24][25] Research has found that in recent decades the sea surface temperatures has risen up by Script error: No such module "convert". in the Arabian Sea.[25] During Cyclone Amphan’s rapid intensification, sea surface temperatures were as high as Template:Cvt in the Bay of Bengal, and parts of the Arabian Sea reached Template:Cvt before the formation of Cyclone Nisarga.[26] According to the Union Ministry of Earth and Science, the frequency of very severe cyclonic storms has risen up by one per decade in last two decades, despite the decrease of the overall tropical cyclone frequency in the same period.[25] Higher temperatures caused the cyclones to become more powerful and lead to tropical cyclone formation faster. Rising sea level also caused higher storm surge.[26] Researchers also predict that cyclones will be deadlier and stronger as the trend of warming sea surface temperatures continue. Rising sea levels also may cause severe flooding, strong storm surge and inundation of coastal towns.[26]

Seasons

Historical storm formation by month between 1990 and 2020
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Before 1890

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1890s

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Year D CS SCS Notes
1890 10 4 1
1891 13 4 3 Total includes 1 Land Severe Cyclonic Storm
1892 12 7 2
1893 12 10 4
1894 12 6 0
1895 11 5 4
1896 10 8 3
1897 12 6 8
1898 13 7 3
1899 7 3 0
Total 112 60 28
References[27]

1900s

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Year D CS SCS Strongest
storm
Deaths Damage
(USD)
Notes
1900 10 3 1
1901 6 3 2
1902 13 7 5
1903 14 8 2
1904 9 4 0
1905 10 6 0
1906 11 7 1
1907 15 8 4
1908 9 6 1
1909 8 8 4
Total 105 60 20
References[27]

1910s

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Year D CS SCS Strongest
storm
Deaths Damage
(USD)
Notes
1910 6 5 2
1911 7 5 4
1912 9 6 2
1913 10 6 2
1914 8 4 2
1915 9 6 0
1916 14 8 5
1917 10 3 1
1918 11 5 0
1919 11 6 3
Total 95 54 21
References[27]

1920s

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Year D CS SCS Strongest
storm
Deaths Damage
(USD)
Notes
1920 9 5 0
1921 10 4 1
1922 13 6 6
1923 16 4 3
1924 13 6 0
1925 20 7 3
1926 13 10 3
1927 18 7 2
1928 13 7 0
1929 15 6 0
Total 140 62 18
References[27]

1930s

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Year D CS SCS Strongest
storm
Deaths Damage
(USD)
Notes
1930 14 10 1
1931 11 5 1
1932 14 6 2
1933 16 8 3
1934 16 5 0
1935 15 6 2
1936 18 6 3 <templatestyles src="Legend/styles.css" /> VSCS Two 293 $75,000
1937 19 6 2
1938 10 4 4
1939 19 7 3
Total 152 63 21
References[27][28]

1940s

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Year D CS SCS Strongest
storm
Deaths Damage
(USD)
Notes
1940 16 8 5
1941 19 8 4
1942 14 5 2
1943 14 7 1
1944 19 8 2
1945 15 3 2
1946 17 5 1
1947 18 4 2
1948 18 6 3
1949 12 1 1
Total 162 55 23
References[27]

1950s

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Year D CS SCS Strongest
storm
Deaths Damage
(USD)
Notes
1950 16 4 0 <templatestyles src="Legend/styles.css" /> SCS  Sixteen Unknown Unknown
1951 15 4 2 <templatestyles src="Legend/styles.css" /> SCS  Fifteen Unknown Unknown
1952 17 4 2
1953 10 1 1
1954 14 1 0
1955 13 6 2
1956 14 4 2
1957 7 4 2
1958 12 5 2
1959 16 6 3
Total 134 39 16 Unknown Unknown
References[27]

1960s

File:Nov319660819zESSA3MadrasCyclone.jpg
This ESSA 3 satellite image was taken on November 3, 1966, at 0819 UTC of a tropical cyclone striking Madras, India
Year D CS SCS Strongest
storm
Deaths Damage
(USD)
Notes
1960 15 5 3 <templatestyles src="Legend/styles.css" /> VSCS  Ten Template:Nts >Template:Ntsp Vast majority of the fatalities resulted from two cyclones striking East Pakistan three weeks apart
1961 18 5 4 <templatestyles src="Legend/styles.css" /> SCS  Winnie Template:Nts Script error: No such module "sort". Three land depressions developed this season
1962 13 5 3 <templatestyles src="Legend/styles.css" /> VSCS  Twelve Template:Nts Template:Ntsp Deadliest storm, Harriet, crossed over from the Western Pacific
1963 17 6 4 <templatestyles src="Legend/styles.css" /> SuCS  Three Template:Nts Script error: No such module "sort".
1964 16 7 5 <templatestyles src="Legend/styles.css" /> SuCS  "Rameswaram" >Template:Nts >Template:Ntsp
1965 14 6 4
1966 18 8 6
1967 15 6 4
1968 13 7 4 <templatestyles src="Legend/styles.css" /> SuCS  "Burma"
1969 14 6 1 <templatestyles src="Legend/styles.css" /> ESCS  Twelve
Total 153 61 38 Three >47,000 >$193.9 million
References[27]

1970s

Year D CS SCS Strongest
storm
Deaths Damage
(USD)
Notes
1970 15 7 3 <templatestyles src="Legend/styles.css" /> ESCS  "Bhola" 300,000-500,000 86.4 million The Bhola cyclone is the deadliest tropical cyclone recorded worldwide
1971 15 7 6 <templatestyles src="Legend/styles.css" /> ESCS  "Odisha"
1972 18 7 6 <templatestyles src="Legend/styles.css" /> ESCS  09B
1973 16 6 3 <templatestyles src="Legend/styles.css" /> SCS  14B
1974 12 7 3 <templatestyles src="Legend/styles.css" /> VSCS  06B
1975 20 7 4 <templatestyles src="Legend/styles.css" /> ESCS  02A
1976 14 10 7 <templatestyles src="Legend/styles.css" /> ESCS  02A
1977 18 5 5 <templatestyles src="Legend/styles.css" /> SuCS  "Andhra Pradesh" up to 50,000 $192 million Devastated Krishna Delta area in Andhra Pradesh
1978 14 5 3 <templatestyles src="Legend/styles.css" /> SuCS  "Sri Lanka" 1,000+
1979 11 5 4 <templatestyles src="Legend/styles.css" /> ESCS  01B
Total 153 66 44 "Andhra Pradesh" >800,000 >$278.4 million
References[27]

1980s

Year D DD CS SCS VSCS ESCS SuCS Strongest
storm
Deaths Damages
(USD)
Notes
1980 14 14 5 0 0 0 0 <templatestyles src="Legend/styles.css" /> CS  BOB 02
1981 12 12 5 3 3 0 0 <templatestyles src="Legend/styles.css" /> VSCS  BOB 03
1982 19 11 8 5 3 3 0 <templatestyles src="Legend/styles.css" /> ESCS  BOB 01
1983 7 4 2 1 1 1 0 <templatestyles src="Legend/styles.css" /> CS  Herbert
1984 7 7 4 3 3 2 0 <templatestyles src="Legend/styles.css" /> ESCS  "Sriharikota" 430
1985 15 15 6 1 1 0 0 <templatestyles src="Legend/styles.css" /> VSCS  "Bangladesh" 11,107
1986 8 3 1 0 0 0 0 <templatestyles src="Legend/styles.css" /> CS  02B 11
1987 9 8 5 3 1 0 0 <templatestyles src="Legend/styles.css" /> VSCS  01B
1988 9 5 5 3 2 2 0 <templatestyles src="Legend/styles.css" /> ESCS  "Bangladesh" 6,740 $13 million
1989 10 5 3 2 1 1 1 <templatestyles src="Legend/styles.css" /> SuCS  Gay 1,785 $25.27 million Typhoon Gay crossed over from the West Pacific Basin
Total 110 84 44 21 15 9 1 Gay / Kavali >20,073 >$38.27 billion
References[27]

1990s

File:Cyclone 05B.jpg
The 1999 Odisha Cyclone making landfall over Odisha in 1999.
Year D DD CS SCS VSCS ESCS SuCS Strongest
storm
Deaths Damage
(USD)
Notes and References
1990 11 6 2 2 1 1 1 <templatestyles src="Legend/styles.css" /> SuCS  BOB 01 Template:Nts Template:Ntsp [29][30]
1991 9 4 3 1 1 1 1 <templatestyles src="Legend/styles.css" /> SuCS  "Bangladesh" Script error: No such module "sort". Template:Ntsp [30]
1992 13 11 7 2 1 1 0 <templatestyles src="Legend/styles.css" /> ESCS  Forrest Script error: No such module "sort". Template:Ntsp Forrest crossed over from the West Pacific Basin
1993 5 4 2 2 2 0 0 <templatestyles src="Legend/styles.css" /> ESCS  BOB 02 Script error: No such module "sort". Template:Ntsp
1994 5 5 4 2 2 1 0 <templatestyles src="Legend/styles.css" /> ESCS  "Bangladesh" Script error: No such module "sort". Template:Ntsp
1995 8 6 3 2 2 1 0 <templatestyles src="Legend/styles.css" /> ESCS  BOB 07 Script error: No such module "sort". Template:Ntsp
1996 10 8 6 4 2 0 0 <templatestyles src="Legend/styles.css" /> VSCS  "Andhra Pradesh" Script error: No such module "sort". Template:Ntsp
1997 9 7 3 2 1 1 0 <templatestyles src="Legend/styles.css" /> ESCS  "Bangladesh" Script error: No such module "sort". Unknown
1998 13 10 6 5 3 1 0 <templatestyles src="Legend/styles.css" /> ESCS  "Gujarat" Script error: No such module "sort". Template:Ntsp
1999 10 8 5 3 3 2 1 <templatestyles src="Legend/styles.css" /> SuCS  "Odisha" Script error: No such module "sort". Template:Ntsp The Odisha cyclone is the strongest cyclone recorded in the Northern Indian Ocean.
Total 93 69 41 25 18 9 3 "Odisha" >168,923 ~$12.35 billion
References[27]

2000s

File:Gonu 2007-06-04 0900Z.jpg
Cyclone Gonu at its peak in 2007.
Year D DD CS SCS VSCS ESCS SuCS Strongest
storm
Deaths Damage
(USD)
Notes
2000 7 6 5 2 2 2 0 <templatestyles src="Legend/styles.css" /> ESCS  "South India" Script error: No such module "sort". Template:Ntsp
2001 6 5 4 1 1 1 0 <templatestyles src="Legend/styles.css" /> ESCS  "Gujarat" Script error: No such module "sort". Template:Ntsp
2002 7 7 4 1 0 0 0 <templatestyles src="Legend/styles.css" /> SCS  "West Bengal" Script error: No such module "sort". Template:Ntsp
2003 7 5 3 3 1 0 0 <templatestyles src="Legend/styles.css" /> VSCS  "Sri Lanka" Script error: No such module "sort". Template:Ntsp
2004 10 7 4 4 1 1 0 <templatestyles src="Legend/styles.css" /> ESCS  "Myanmar" Script error: No such module "sort". Template:Ntsp
2005 12 7 3 0 0 0 0 <templatestyles src="Legend/styles.css" /> CS  Pyarr Script error: No such module "sort". Template:Ntsp
2006 12 6 3 2 1 1 0 <templatestyles src="Legend/styles.css" /> ESCS  Mala Script error: No such module "sort". Template:Ntsp
2007 11 8 4 2 2 2 1 <templatestyles src="Legend/styles.css" /> SuCS  Gonu Script error: No such module "sort". Template:Ntsp
2008 10 7 4 1 1 1 0 <templatestyles src="Legend/styles.css" /> ESCS  Nargis Script error: No such module "sort". Template:Ntsp The deadliest cyclone season since 1970
Second-costliest cyclone season on record
2009 8 6 4 1 0 0 0 <templatestyles src="Legend/styles.css" /> SCS  Aila Script error: No such module "sort". Template:Ntsp
Total 90 64 38 17 9 8 1 Gonu >157,965 $16.65 billion
References[27]

2010s

File:Kyarr 2019-10-27 0858Z.jpg
Cyclone Kyarr was the first super cyclone since 2007.
Year D DD CS SCS VSCS ESCS SuCS Strongest
storm
Deaths Damages
(USD)
Notes
2010 8 6 5 4 2 1 0 <templatestyles src="Legend/styles.css" /> ESCS  Giri 402 Template:Ntsp The most active season since 1998
2011 10 6 2 1 1 0 0 <templatestyles src="Legend/styles.css" /> VSCS  Thane 360 Template:Ntsp
2012 5 5 2 0 0 0 0 <templatestyles src="Legend/styles.css" /> CS  Nilam 128 Template:Ntsp The first depression of the year did not develop until October 10
2013 10 6 5 4 3 1 0 <templatestyles src="Legend/styles.css" /> ESCS  Phailin 323 Template:Ntsp Featured Phailin, the first Category 5-equivalent cyclone since Sidr in 2007
2014 8 5 3 2 2 2 0 <templatestyles src="Legend/styles.css" /> ESCS  Nilofar 183 Template:Ntsp
2015 12 9 4 2 2 2 0 <templatestyles src="Legend/styles.css" /> ESCS  Chapala 363 Template:Ntsp First season on record with two cyclones producing hurricane-force winds in Socotra
2016 10 5 4 1 1 0 0 <templatestyles src="Legend/styles.css" /> VSCS  Vardah 401 Template:Ntsp
2017 10 6 3 2 1 0 0 <templatestyles src="Legend/styles.css" /> VSCS  Ockhi 834 Template:Ntsp
2018 14 9 7 5 3 1 0 <templatestyles src="Legend/styles.css" /> ESCS  Mekunu 343 Template:Ntsp The most active season since 1992
2019 12 11 8 6 6 3 1 <templatestyles src="Legend/styles.css" /> SuCS  Kyarr 173 Template:Ntsp Earliest cyclonic storm in the basin
First Super Cyclonic Storm since 2007
Total 99 68 43 27 21 10 1 Kyarr 3510 Template:Ntsp
References[27]

2020s

File:Amphan 2020-05-18 0745Z.jpg
Amphan was the costliest cyclone in the basin to strike land.
Year D DD CS SCS VSCS ESCS SuCS Strongest
storm
Deaths Damages
(USD)
Notes
2020 9 6 5 4 3 1 1 <templatestyles src="Legend/styles.css" /> SuCS  Amphan 269 Template:Ntsp First super cyclonic storm in the Bay of Bengal since 1999
Featured the costliest cyclone ever recorded in the basin, Amphan
Costliest North Indian cyclone season on record
2021 10 6 5 3 2 1 0 <templatestyles src="Legend/styles.css" /> ESCS  Tauktae 230 $5.31 billion
2022 15 7 3 2 0 0 0 <templatestyles src="Legend/styles.css" /> SCS  Asani 79 $52.4 million

First season on record to have two depressions forming in the month of March

2023 10 8 7 5 4 3 0 <templatestyles src="Legend/styles.css" /> ESCS Mocha 523 $1.07 billion Mocha was one of the strongest cyclones ever formed in the basin's history.
2024 12 7 4 2 0 0 0 <templatestyles src="Legend/styles.css" /> SCS  Remal 279 $2.29 billion
2025 1 0 0 0 0 0 0 None None
Total 57 34 24 16 9 5 1 Amphan 1,380 $24.52 billion

Records

See also

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Notes

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References

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