2024 North Indian Ocean cyclone season | |
---|---|
Seasonal boundaries | |
First system formed | 24 May 2024 |
Last system dissipated | Season ongoing |
Strongest storm | |
Name | Remal |
• Maximum winds | 110 km/h (70 mph) (3-minute sustained) |
• Lowest pressure | 978 hPa (mbar) |
Seasonal statistics | |
Depressions | 10 |
Deep depressions | 6 |
Cyclonic storms | 3 |
Severe cyclonic storms | 2 |
Total fatalities | 227 total |
Total damage | $630 million (2024 USD) |
Related articles | |
The 2024 North Indian Ocean cyclone season is an ongoing event in the annual cycle of tropical cyclone formation. It has been unreasonably less active in terms of formation of cyclonic storms. [1] The season has no official bounds, but cyclones tend to form between April and December, with the peak from May to Early November. These dates conventionally delimit each year when most tropical cyclones form in the northern Indian Ocean.
The scope of this article 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 this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center (JTWC) releases unofficial advisories. On average, three to four cyclonic storms form in this basin every season. [2]
Severe cyclonic storm (IMD) | |
Tropical storm (SSHWS) | |
Duration | 24 May – 28 May |
---|---|
Peak intensity | 110 km/h (70 mph) (3-min); 978 hPa (mbar) |
After four months of inactivity, on 21 May, the India Meteorological Department (IMD) began monitoring a cyclonic circulation in the Bay of Bengal. [3] Later that day, the Joint Typhoon Warning Center (JTWC) would also begin tracking the system, noting that it was likely to become a monsoon depression. [4] The next day, the IMD noted that a low-pressure area had formed adjacent to the cyclonic circulation. [5] Late on 23 May, the IMD upgraded the system into a well-marked low, stating that it was rapidly coalescing. [6] The next day, the IMD stated that the depression formed in the Bay of Bengal, designating it as BOB 01. [7] Subsequently, the JTWC issued a Tropical Cyclone Formation Alert (TCFA), noting the depression's broad circulation center and its improving rainbands. [8] The next day, BOB 01 intensified into a deep depression. [9] The JTWC would recognize the system as a cyclone, designating it as 01B. [10] Soon after, the depression intensified into a cyclonic storm, causing the IMD to name it Remal. [11] On 26 May, Remal intensified into a severe cyclonic storm with 3-minute sustained winds of 95 km/h (60 mph). Due to favourable conditions, including high sea surface temperatures over northern Bay of Bengal and low wind shear, Remal intensified further with wind speeds reaching 110 km/h. It made landfall over Bangladesh and adjoining West Bengal on the night of 26 May. Landfall process had been completed by the morning of 27 May and had weakened into a cyclonic storm.
Depression (IMD) | |
Duration | 19 July – 20 July |
---|---|
Peak intensity | 45 km/h (30 mph) (3-min); 990 hPa (mbar) |
On 19 July, IMD marked an area of low pressure off the coast of Odisha. The disturbance was later upgraded into a depression, designated as BOB 02. [12] The disturbance later moved inland, weakened back into a low-pressure area. [13]
Deep depression (IMD) | |
Duration | 2 August – 6 August |
---|---|
Peak intensity | 55 km/h (35 mph) (3-min); 995 hPa (mbar) |
On 31 July, a cyclonic circulation formed over Gangetic West Bengal. Tracking westward, on 2 August, the disturbance developed into a depression. Two days later, it intensified further, becoming a deep depression over southwest Bihar. [14] Continuing its westward track, on 5 August, the system weakened into a depression. [15] It dissipated the next day. [16]
Due to the westward shift of the monsoon trough, the depression formed on land instead of the usual formation in the Bay of Bengal. [17]
As a result of the depression, Dum Dum in Kolkata received 100 millimetres (3.9 in) of rain on 3 August. [18]
Cyclonic storm (IMD) | |
Tropical storm (SSHWS) | |
Duration | 25 August – 3 September |
---|---|
Peak intensity | 75 km/h (45 mph) (3-min); 988 hPa (mbar) |
On 24 August, a cyclonic circulation formed over Madhya and Uttar Pradesh. Early the next day, on 25 August, the IMD noted that it had developed into a land depression over Rajasthan and Madhya Pradesh. [19] Later that day, the depression intensified into a deep depression southeast of Udaipur. [20] On 27 August, the JTWC began tracking the deep depression, noting that it was in a marginal environment for development. [21] Two days later, on 29 August, they issued a TCFA on the developing depression, [22] prior to designating it as Tropical Cyclone 02A early the next day. [23] Later that same day, on 30 August, the IMD upgraded it into a cyclonic storm, naming it Asna. [a] [25] [26] It further moved into the Arabian Sea. [27] On 1 September, Asna was stripped of any convection due to dry air entrainment and degenerated to a remnant low. [28]
Many parts of Gujarat and Madhya Pradesh were flooded due to heavy rains from the storm. p to 260 mm (10 in) of rain fell in Vadodara and Ahmedabad recorded 120 mm (4.7 in) of rainfall. [29] [30] Flooding in Gujarat killed 49 people. [31] [32] An initial survey reported that the Government of Gujarat suffered damages worth more than ₹250 crore (US$30 million) to government properties and public infrastructure. [33]
Depression (IMD) | |
Duration | 31 August – 2 September |
---|---|
Peak intensity | 45 km/h (30 mph) (3-min); 996 hPa (mbar) |
On 29 August, the IMD marked an area of low pressure in the Bay of Bengal. Two days later, early on 31 August, the IMD upgraded it into a depression, designated as BOB 03, off the coast of Andhra Pradesh. It made landfall that same day before weakening back to a low pressure inland.
27 deaths from rain related incidents were recorded in Andhra Pradesh and Telangana. [34]
Deep depression (IMD) | |
Duration | 7 September – 13 September |
---|---|
Peak intensity | 55 km/h (35 mph) (3-min); 990 hPa (mbar) |
Late on 5 September, the IMD marked an area of low pressure in the Bay of Bengal. On 7 September, it got upgraded to a depression by the IMD and marked as Invest 92B by the JTWC. Then, on 8 September, it got upgraded to a deep depression off the coast of Odisha. On 9 September, the deep depression made landfall in Odisha and weakened back down to a prominent low pressure system. Two days later, the IMD reupgraded the system into a depression over Madhya Pradesh. On 13 September, the depression finally dissipated over northwest Uttar Pradesh.
Deep depression (IMD) | |
Duration | 13 September – 18 September |
---|---|
Peak intensity | 55 km/h (35 mph) (3-min); 989 hPa (mbar) |
After degenerating into a remnant low, the weak remnants of Typhoon Yagi would begin tracking towards the North Indian Ocean, [35] causing the IMD to start tracking it as a cyclonic circulation over Myanmar on 11 September. [36] This disturbance would coalesce into a low-pressure area the next day, [37] further developing into a well-marked low-pressure just a few hours later. [38] Soon after, it developed into a depression. [39] Early the next morning, it became a deep depression over Bangladesh and West Bengal. [40] On 15 September, it weakened back down to a depression as it slowly moved westwards over western India.
Due to heavy rain from this system, seven people were killed by landslides in Cox's Bazar District. [41] Five fishermen also died [42] and over 500 more went missing in the district. [43] In Cox's Bazar, 378 mm (14.9 in) of rain was recorded within a 12-hour period from 11 to 12 September. [44] These heavy rains resulted in the flooding of over 200 villages within seven upazilas of the district. [42] Another 11 people were killed by flooding in Noakhali District, [45] where 100 fishermen went missing. Additionally, two people were killed when a boat capsized in Jagannathpur Upazila. [46] In India, heavy rains lashed Kolkata and West Bengal. 72.4 mm (2.85 in) of rain was recorded over a 24-hour period, with a total of 125.8 mm (4.95 in) was recorded in Kolkata. [47]
Due to the heavy rains, the Damodar Valley Corporation released more than 3.5 lakh cusec of water from its dams, resulting in inundation of Birbhum, Bankura, Howrah, Hooghly, North and South 24 Parganas, Purba and Paschim Medinipur, and Paschim Bardhaman districts of West Bengal. 28 people were killed due to these floods and 25,000 people had to moved to safer areas. [48]
Depression (IMD) | |
Duration | 13 October – 15 October |
---|---|
Peak intensity | 45 km/h (30 mph) (3-min); 1004 hPa (mbar) |
On 11 October, the IMD marked an area of low pressure in the Arabian Sea. Two days later, late on 13 October, the IMD upgraded it into a depression, designated as ARB 01. On 15 October, it degenerated back to a low pressure due to increased dry air making it more disorganized. Later that same day, it stalled over the coast of Oman before dissipating on 16 October.
Depression (IMD) | |
Duration | 15 October – 17 October |
---|---|
Peak intensity | 45 km/h (30 mph) (3-min); 1002 hPa (mbar) |
On 14 October, a well marked low pressure area formed in the south of the Bay of Bengal. The IMD upgraded it to a depression, designating it as BOB 06, early on 15 October as it moved west-northwestwards before making landfall in Andhra Pradesh on 17 October at 04:30 IST. It weakened further into a low pressure area as it moved north-westwards into India and dissipated. [49]
In the wake of this system, heavy rains slashed Puducherry, Chennai and other parts of Andhra Pradesh, bringing these areas to a standstill. Bengaluru and its adjoining areas too received heavy rainfall. Residential neighbourhoods and roads were inundated with knee-deep water, causing widespread disruptions to daily life. The relentless downpour led to traffic congestion, crippled public transportation services, and forced the cancellation of several flights. The Southern Railway announced the cancellation and diversion of several trains due to waterlogging. [50]
Severe cyclonic storm (IMD) | |
Category 1 tropical cyclone (SSHWS) | |
Duration | 22 October – 26 October |
---|---|
Peak intensity | 110 km/h (70 mph) (3-min); 984 hPa (mbar) |
A low pressure area formed in the south Bay of Bengal at 23:30 IST on October 20. It moved northwestwards and formed a well marked low pressure area at 11:30 IST on October 21. It concentrated into a depression at 05:30 IST on October 22, 770 km south-southeast of Sagar Island. [51] At 16:30 IST, JTWC issued a TCFA on the depression. By 17:30 IST, it had consolidated into a deep depression and was 740 km south-southeast of Sagar Island, moving in a west-northwestern direction at a speed of 7 km/h. [52] Over the next 6 hours, it intensified into cyclonic storm Dana [b] ( /ˈdɑːnə/ ); moving with a speed of 18 km/h and lay centered 630 km from of Sagar Island at 05:30 IST of October 23. It further intesified into a severe cyclonic storm at 23:30 IST; moving at a speed of 15 km/h and lay centered about 420 km from Sagar Island. [54] The storm made landfall between 23:30 IST of October 24 and 08:30 IST of October 25 close to Habalikhati Nature Camp (Bhitarkanika) and Dhamra Port on the Odisha Coast, subsequently weakening into a cyclonic storm. [55] It weakened further into a deep depression with wind speeds of 55 km/h and gusts of 75 km/h and at 14:30 IST it was 40 km north-northwest of Bhadrak. [56] Then it weakened into a depression about 70 km east-southeast of Keonjhar at 23:30 IST and remained stationary over that area, weakening further into a remnant low and dissipated. [57]
Within this basin, a tropical cyclone is assigned a name when it is judged to have reached cyclonic storm intensity with winds of 65 km/h (40 mph). The names were selected by a new list from the Regional Specialized Meteorological Center in New Delhi by mid-2020. [58] There is no retirement of tropical cyclone names in this basin as the list of names is only scheduled to be used once before a new list of names is drawn up. Should a named tropical cyclone move into the basin from other basins, then it will retain its original name. The next five available names from the list of North Indian Ocean storm names are below. [59]
|
This is a table of all storms in the 2024 North Indian Ocean cyclone season. It mentions all of the season's storms and their names, duration, peak intensities according to the IMD storm scale, damage, and death totals. Damage and death totals include the damage and deaths caused when that storm was a precursor wave or extratropical low. All of the damage figures are in 2024 USD.
Name | Dates | Peak intensity | Areas affected | Damage (USD) | Deaths | Refs | ||
---|---|---|---|---|---|---|---|---|
Category | Wind speed | Pressure | ||||||
Remal | 24–28 May | Severe cyclonic storm | 110 km/h (70 mph) | 978 hPa (28.88 inHg) | India (Odisha, West Bengal, Jharkhand, Northeast India), Bangladesh, Myanmar | $600 million | 84 | [60] |
BOB 02 | 19–20 July | Depression | 45 km/h (30 mph) | 990 hPa (29.23 inHg) | Odisha | None | None | |
LAND 01 | 2–6 August | Deep depression | 55 km/h (35 mph) | 995 hPa (29.38 inHg) | West Bengal, Jharkhand, Bihar, Uttar Pradesh, Madhya Pradesh, Rajasthan | None | None | |
Asna | 25 August – 3 September | Cyclonic storm | 75 km/h (45 mph) | 988 hPa (29.18 inHg) | Madhya Pradesh, Rajasthan, Gujarat, Pakistan | $30 million | 73 | [33] |
BOB 03 | 31 August – 2 September | Depression | 45 km/h (30 mph) | 996 hPa (29.41 inHg) | Andhra Pradesh, Telangana, Odisha | None | 27 | |
BOB 04 | 7–13 September | Deep depression | 55 km/h (35 mph) | 990 hPa (29.23 inHg) | Odisha, Madhya Pradesh, Uttar Pradesh | None | None | |
BOB 05 | 13–18 September | Deep depression | 55 km/h (35 mph) | 989 hPa (29.21 inHg) | Bangladesh, West Bengal, Jharkhand, Chhattisgarh, Madhya Pradesh, Uttar Pradesh | None | 27 (350+ missing) | |
ARB 01 | 13–15 October | Depression | 45 km/h (30 mph) | 1004 hPa (29.65 inHg) | Oman | None | None | |
BOB 06 | 15–17 October | Depression | 45 km/h (30 mph) | 1002 hPa (29.59 inHg) | Tamil Nadu, Andhra Pradesh, Puducherry, Karnataka | None | None | |
Dana | 22 October–26 October | Severe cyclonic storm | 110 km/h (70 mph) | 984 hPa (29.06 inHg) | Odisha, West Bengal, Chhattisgarh, Jharkhand, Karnataka, Andhra Pradesh, Bangladesh | Minimal | 17+ | |
Season aggregates | ||||||||
10 systems | 24 May – Season ongoing | 110 km/h (70 mph) | 978 hPa (28.88 inHg) | $630 million | 227 |
The 2007 North Indian Ocean cyclone season was one of the most active North Indian Ocean cyclone seasons on record. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
The 2008 North Indian cyclone season was one of the most disastrous tropical cyclone seasons in modern history, causing more than 140,000 fatalities and over US$15 billion in damage. At the time, it was the costliest season in the North Indian Ocean, until it was surpassed by 2020. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal, which is east of India, and the Arabian Sea, which is west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), however the Joint Typhoon Warning Center releases unofficial advisories for military interests. An average of four to six storms form in the North Indian Ocean every season. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD.
Below is a timeline of the 2007 North Indian Ocean cyclone season, documenting major events with regards to tropical cyclone formation, strengthening, weakening, landfall, extratropical transition, as well as dissipation. The 2007 North Indian Ocean cyclone season was an ongoing event in the annual cycle of tropical cyclone formation.
The 2009 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
Cyclonic Storm Nisha was a fairly weak but catastrophic tropical cyclone that struck Sri Lanka, and India which killed over 200. It was the ninth tropical cyclone of the 2008 North Indian Ocean cyclone season, and the seventh tropical cyclone in the Bay of Bengal that year.
The 2010 North Indian Ocean cyclone season was one of the most active tropical cyclone season in the North Indian Ocean since 1998. The season saw 8 depressions and 5 named storms forming in the region.
Cyclonic Storm Phyan developed as a tropical disturbance to the southwest of Colombo in Sri Lanka on November 4, 2009. Over the next couple of days, the disturbance gradually developed before weakening as it made landfall on Southern India on November 7. After the disturbance emerged into the Arabian Sea, it rapidly became more of a concern to the India Meteorological Department (IMD) reporting early on November 9 that the disturbance had intensified into a Depression, and designated it as Depression ARB 03 whilst the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert. Later that day, the JTWC designated the system as Cyclone 04A. During the next day, the Depression turned towards the northeast the IMD reported that it had intensified into a Cyclonic Storm and named it as Phyan.
The 2011 North Indian Ocean cyclone season was the least active tropical cyclone season in the North Indian Ocean since 1993. Only two cyclonic storms formed, below the average of four to six. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article 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 2012 North Indian Ocean cyclone season was a very inactive season. The season had a very late start, with the first system forming in October. During the season, only five systems formed, of which only two became cyclonic storms. Both the storms made landfall, and they, along with the deep depressions, were responsible for 128 deaths and economic losses worth at least $56.7 million.
Very Severe Cyclonic Storm Thane was the strongest tropical cyclone of 2011 within the Bay of Bengal. Thane initially developed as a tropical disturbance within the monsoon trough to the west of Indonesia. Over the next couple of days the disturbance gradually developed further while moving towards the northwest, and was declared a Depression during December 25, before being named Cyclonic Storm Thane the next day. Thane started to turn towards the west under the influence of a subtropical ridge of high pressure before its development slowed during December 27, as a strong outflow and marginally favourable sea surface temperatures fought with persistent vertical wind shear. After its development had slowed during December 27, Thane became a Very Severe Cyclonic Storm during December 28, before as it approached the Indian states of Tamil Nadu, it weakened slightly. Thane then made landfall early on December 30, on the north Tamil Nadu coast between Cuddalore and Puducherry and rapidly weakened into a depression.
The 2012 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The scope of this article 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 this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center releases unofficial advisories. This timeline includes information that was operationally released, meaning that data from post-storm reviews by the IMD, such as a storm that was not operationally warned upon, has not been included. This timeline documents tropical cyclone formations, strengthening, weakening, landfalls, and dissipations during the season.
The 2013 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones formed in the North Indian Ocean and Arabian Sea. The season had no official bounds, but cyclones typically formed between May and December, with the peak from October to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
The 2014 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The season included two very severe cyclonic storms, both in October, and one other named cyclonic storm, classified according to the tropical cyclone intensity scale of the India Meteorological Department. Cyclone Hudhud is estimated to have caused US$3.58 billion in damage across eastern India, and more than 120 deaths.
The 2015 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between months of April and December, with the peak from May to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
The 2016 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. It was the deadliest season since 2010, killing more than 400 people. The season was an average one, seeing four named storms, with one further intensifying into a very severe cyclonic storm. The first named storm, Roanu, developed on 19 May while the season's last named storm, Vardah, dissipated on 18 December. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the two peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
The 2020 North Indian Ocean cyclone season was the costliest North Indian Ocean cyclone season on record, mostly due to the devastating Cyclone Amphan. 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. The 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 would break 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 2021 North Indian Ocean cyclone season was an average season, the North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, peaking between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The season began on April 2, when a depression designated as BOB 01 was formed in the north Andaman Sea and quickly made landfall in Myanmar. The basin remained quiet for over a month before Cyclone Tauktae formed. It rapidly intensified into an extremely severe cyclonic storm before making landfall in Gujarat, become the strongest storm ever to strike that state since the 1998 Gujarat cyclone. Later that month, BOB 02 formed and later strengthened into Cyclone Yaas. Yaas rapidly intensified into a very severe cyclonic storm before making landfall in northwestern Odisha. The season's strongest tropical cyclone was Cyclone Tauktae, with maximum wind speeds of 185 km/h (115 mph) and a minimum barometric pressure of 950 hPa (28.05 inHg).
The 2022 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. It was an above-average season in terms of depressions and average in terms of deep depressions, but slightly below average in terms of cyclonic storms. It was also the least deadly North Indian Ocean cyclone season since 1988, according to official data. The season's strongest tropical cyclone was Cyclone Asani, with maximum wind speeds of 100 km/h and a minimum barometric pressure of 982 hPa. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the peak from May to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
The 2023 North Indian Ocean cyclone season was a highly above-average and deadly season, becoming the most active since 2019, with nine depressions and six cyclonic storms forming. It was the deadliest since 2017, mostly due to Cyclone Mocha, and had the second-highest accumulated cyclone energy (ACE) in the basin, after 2019. It also had the most extremely severe cyclonic storms on record, tying with 1999 and 2019. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the peak from May to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. However, a cyclone can form at any time during the year shown by an unnamed depression that affected Sri Lanka in January–February.
Severe Cyclonic Storm Asani was a strong tropical cyclone that made landfall in India in May 2022. It was the strongest storm of 2022 North Indian Ocean cyclone season. The third depression and deep depression, and the first named storm of the 2022 North Indian Ocean cyclone season, Asani originated from a depression that the Indian Meteorological Department first monitored on May 7. Conditions rapidly favored development as the system became a deep depression by that day before intensifying to a Cyclonic Storm Asani. On the next day it further intensified and peak to a severe cyclonic storm, before making landfall as a deep depression system over Andhra Pradesh. It degenerated into a well marked low-pressure on May 12.
{{cite report}}
: CS1 maint: url-status (link){{cite report}}
: CS1 maint: url-status (link){{cite report}}
: CS1 maint: url-status (link){{cite report}}
: CS1 maint: url-status (link)