Meteorological history | |
---|---|
Formed | 4 February 2023 |
Dissipated | 14 March 2023 |
Duration | 5 weeks and 3 days (Longest-lasting tropical system on record) |
Very intense tropical cyclone | |
10-minute sustained (MFR) | |
Highest winds | 230 km/h (145 mph) |
Lowest pressure | 927 hPa (mbar);27.37 inHg |
Category 5-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 260 km/h (160 mph) |
Lowest pressure | 923 hPa (mbar);27.26 inHg |
Overall effects | |
Areas affected |
|
Part of the 2022–23 Australian region and South-West Indian Ocean cyclone seasons | |
History • Meteorological history Response • Commons:Freddy images |
Cyclone Freddy was the longest-lived tropical cyclone,lasting five weeks and three days,surpassing the previous record holder,1994's Hurricane John. It also had the highest accumulated cyclone energy,a metric used to measure tropical cyclone activity,ever recorded worldwide. It also featured a record seven separate rounds of rapid intensification during February and March 2023. Freddy originated from a tropical low south of the Indonesian archipelago early on 4 February. Deep convection soon developed,and the system intensified Category 1 tropical cyclone on the Australian scale on 6 February. Located just within Tropical Cyclone Warning Centre Melbourne's area of responsibility,the storm was named Freddy—the third named storm of the 2022–23 Australian region cyclone season—by the Australian Bureau of Meteorology. As it moved westward across the Indian Ocean,Freddy quickly intensified and became a Category 4 severe tropical cyclone before it moved into the area of responsibility of Météo-France La Réunion. As the second very intense tropical cyclone of the 2022–23 South-West Indian Ocean cyclone season. Freddy peaked with 10-minute sustained winds of 230 km/h (145 mph) and a central barometric pressure of 927 hPa (27.37 inHg). It quickly strengthened,reaching 1-minute sustained winds of 270 km/h (165 mph),making it a Category 5-equivalent intensity on the Saffir–Simpson scale.
After briefly weakening from its peak intensity,the cyclone moved toward the northern Mascarene Islands. It then developed a pinhole eye while approaching Madagascar as a compact tropical cyclone. The cyclone then made landfall as a strong Category 2-equivalent intensity with 1-minute sustained winds of 175 km/h (110 mph) near Mananjary,Madagascar on 21 February. This made Freddy the strongest storm to impact the island nation since Cyclone Batsirai a year earlier. It weakened further as it moved overland but regained strength upon reaching the Mozambique Channel. The cyclone intensified into a severe tropical storm and then passed north of Europa Island. The cyclone then made its second landfall near Vilankulos,Mozambique,as a moderate tropical storm status on 24 February. Upon re-entering the channel early on 1 March,it began regaining tropical characteristics and meandering along the Madagascar coast. It then intensified into a tropical cyclone with winds of about 175 km/h (110 mph) before making its final landfall near Quelimane,Mozambique on 11 March. Thereafter,it gradually weakened and dissipated late on 14 March.
The origins of Cyclone Freddy can be traced back to 4 February 2023,when the Australian Bureau of Meteorology (BoM) [nb 1] reported that a tropical low—identified as 13U—had formed during an active phase of the Madden–Julian oscillation in conjunction with an equatorial Rossby wave, [2] while it was situated to the south of the Indonesian archipelago. [3] Soon after,the United States Joint Typhoon Warning Center (JTWC) [nb 2] issued a tropical cyclone formation alert,noting that the disturbance was located in a favorable environment with low wind shear and sea surface temperatures of 29–30 °C (84–86 °F). [5] Early on 6 February,the JTWC began issuing warnings on the system,classifying it as Tropical Cyclone 11S. [6] Deep convection increased and the system became a Category 1 tropical cyclone on the Australian scale by 12:00 UTC;the BoM assigned it the name Freddy accordingly. [2] [7] Freddy then rapidly intensified and developed an eye feature on microwave imagery. As a result,the JTWC classified it as a Category 2-equivalent intensity on the Saffir-Simpson scale around 15:00 UTC on 7 February. [8] After its first peak,the system became increasingly susceptible to wind shear and dry air intrusion, [9] causing Freddy to weaken back into a minimal tropical storm by 09:00 UTC on 9 February. [10] Freddy's deep convection around the storm's center had significantly decreased. [2]
Atmospheric conditions became more favorable for development as wind shear decreased and deep convection began to consolidate and wrap around the cyclone. [2] Consequently,the cyclone quickly restrengthened with the storm becoming a Category 3 severe tropical cyclone—attaining an initial peak intensity with winds of 150 km/h (90 mph)—and at 18:00 UTC on 11 February,Freddy reached its second peak intensity as a high-end Category 4 severe tropical cyclone in the Australian basin,with winds of 175 km/h (110 mph) and a central barometric pressure of 951 hPa (28.08 inHg). [2] The cyclone's eyewall displayed cloud tops warming to below −130 °F (−90 °C) while passing over warm sea surface temperature of 29 °C (84 °F). [11] The cyclone's structure continued to gradually weaken before moving over the South-West Indian Ocean. [2] At around 12:00 UTC on 14 February,the BoM passed the responsibility of tracking the system over to the Météo-France office on La Réunion (MFR). [nb 3] Thus,the system was initially classified as a tropical cyclone status before being later upgraded to intense tropical cyclone status around 18:00 UTC that day. [13] [14] A 2023 study published by the American Geophysical Union found that Freddy's southwestward trajectory was driven by a northerly steering flow caused by its interaction with Cyclone Dingani to the west. [15]
Cyclone Freddy acquired annular characteristics on 14 February,bearing a symmetrical appearance and a well-defined 11.5 miles (18.5 km) wide pinhole eye,which was largely surrounded by central dense overcast. [16] On 15 February at 03:00 UTC,the JTWC reported that the cyclone re-strengthened and underwent another period of rapid intensification,reaching Category 4-equivalent intensity; [17] post-analysis by the JTWC revealed that the cyclone had already reached Category 5-equivalent intensity, [18] with 1-minute sustained winds of 270 km/h (165 mph). [19] After maintaining Category 5 intensity for about 12 hours,Freddy weakened slightly before restrengthening back to Category 5 intensity on 19 February. [18] The cyclone's cloud tops warmed to −101 °F (−74 °C), [20] causing the system to display annular characteristics. Additionally,the storm's eye expanded to a diameter of 29 miles (46 km). [21] Concurrently,the cyclone was assigned a T7.0 rating via the Dvorak technique—a method of determining a tropical cyclone's intensity based on satellite appearance. [20] Around 00:00 UTC that day,the MFR upgraded Freddy to a very intense tropical cyclone estimated a minimum barometric pressure of 931 hPa (27.49 inHg) and 10-minute sustained winds of 220 km/h (140 mph). [20] However,in the best track for Freddy,the MFR concluded a peak wind speed of 230 km/h (145 mph),and minimum central pressure of 927 hPa (27.37 inHg). [22] The cyclone then turned west-southwestward,along the northern edge of a mid-level subtropical high. [23]
After reaching its peak intensity,the cyclone's eye pattern quickly deteriorated as the cloud tops warmed on 20 February,while it was traversing north of the Mascarene Islands. [24] Later,an eyewall replacement cycle occurred, [25] causing the storm to weaken. [26] Late on 21 February,the cyclone developed a well-defined 7 miles (11 km) pinhole eye while approaching Madagascar as a compact tropical cyclone. [27] Around 18:00 UTC that day,the cyclone made landfall near Mananjary,Madagascar, [28] with the JTWC estimating winds of 175 km/h (110 mph). [29] This made Freddy the strongest storm to impact the island nation since Cyclone Batsirai a year earlier. [30] It then rapidly weakened upon encountering the mountainous terrain of the island nation and was downgraded to overland depression status. [31] After crossing Madagascar,the cyclone's circulation became exposed,and deep convection was stripped away from the center on 22 February. [32] Moving west-northwestward in response to a subtropical ridge to the west, [33] Freddy emerged over the Mozambique Channel on 23 February. [34] Afterwards,the cyclone's convection increased in the northern semicircle,and by around 06:00 UTC,Freddy had strengthened into a moderate tropical storm. [35] Steered by a subtropical ridge to the south, [36] the cyclone moved westward and quickly intensified into a severe tropical storm around 12:00 UTC that day,with convection wrapping around its center. [37] An automated weather station on Europa Island indicated that Freddy had wind gusts up to 93–111 km/h (58–69 mph) after passing north of the island. [38] Around 12:00 UTC on 24 February,the storm made landfall in Mozambique south of Vilankulos,with winds about 85 km/h (50 mph),just below severe tropical storm strength. [39] It then rapidly weakened as it moved westward and further inland,eventually weakening to overland depression status around 18:00 UTC that day. [40] The system's convective activity was concentrated in the southeastern semicircle over Mozambique on 25 February. [41] Freddy's remnant low continued moving into Zimbabwe late on 26 February,where it stayed for a couple of days. [42]
As early as 26 February,the MFR anticipated that a large low-pressure circulation associated with Freddy would move back toward the coast of Mozambique due to the influence of a trough over the southern Mozambique Channel and a near-equatorial ridge to the north. [42] Projections from computer models also indicated that the system would redevelop into a tropical cyclone. [43] Early on 1 March,Freddy emerged again into the channel—benefiting from favorable environmental conditions such as low vertical wind shear,good upper-level divergence, [44] and sea surface temperatures of 28–29 °C (82–84 °F). [45] The cyclone drifted slowly southward and struggled to intensify due to its broad circulation. [46] At 06:00 UTC on 4 March,the MFR upgraded the system to a moderate tropical storm after an advanced scatterometer showed winds of 44 km/h (25 mph) in the southern semicircle. [47] It was also noted that Freddy was tracking towards the eastward—under the increasing influence of the near-equatorial ridge to the north—as it developed a consolidating low-level circulation. [48]
The cyclone further intensified strengthened into a severe tropical storm status as it accelerated eastward toward the coast of Madagascar early on 5 March. [49] Meandering along the Madagascar coast, [50] the cyclone unexpectedly intensified—developing an ill-defined eye—which prompted the MFR to upgrade it to tropical cyclone status with sustained winds of 150 km/h (90 mph) by 12:00 UTC on 7 March. [51] Freddy's eye disappeared from satellite imagery six hours later due to the effects of southern wind shear. [52] The cyclone's motion accelerated and shifted northwestward under the northeastern side of the steering subtropical ridge early on 9 March. [53] The cyclone rapidly weakened to slightly below minimal tropical storm strength due to increased wind shear and dry air intrusion. [53] Despite this, [54] the cyclone managed to steadily quickly—developing banding features. [55] The cyclone rapidly re-strengthened and made landfall for the final time near Quelimane,Mozambique at 18:00 UTC on 11 March, [56] with the JTWC estimated winds of about 175 km/h (110 mph) [57] —featured a well-defined eye within its compact and symmetrical dense overcast. [58] Within two hours,the eye of Freddy disappeared from satellite imagery,and it was estimated to have fallen below tropical cyclone status on 12 March. [59] The JTWC described the cyclone as "a B-reel horror movie that never ends",and concluded,"It may not stay overland for long." [54] The computer models predicted that the cyclone would turn eastward and re-emerge in the channel; [60] however,it ultimately moved northwestward inland, [54] bringing rain to Malawi and Mozambique before dissipating on 14 March. [22]
Freddy's 36-day duration makes it the longest-lasting tropical cyclone to be recorded worldwide,in terms of the number of days maintaining tropical storm status or higher,surpassing Hurricane John's previous record of 31-days in the 1994 season. [3] Additionally,Freddy was the second-farthest traveling tropical cyclone globally,covering a distance of 12,785 km (7,945 mi),which is approximately 33% of the Earth's circumference—just shy of 1994's Hurricane John,which covered 13,180 km (8,190 mi). [3] In addition,it achieved the highest accumulated cyclone energy—a metric used to measure the total energy generated by tropical cyclones—of any tropical cyclone worldwide,with a total of 87.01,exceeding the previous record set by Hurricane Ioke in 2006. [61] It later became the first tropical cyclone to undergo seven separate rounds of rapid intensification. [62] It exceeded the previous records held by Hurricane Norman in 2018,Hurricane Emily in 2005,and 1994's Hurricane John. [63] Further,it was one of only four systems to traverse the entirety of the southern Indian Ocean from east to west;the others were Cyclone Litanne in 1994 as well as Cyclone Leon-Eline and Cyclone Hudah in 2000. [64]
Intense Tropical Cyclone Bondo was the first of a series of six tropical cyclones to impact Madagascar during the 2006–07 South-West Indian Ocean cyclone season. Bondo developed on 15 December in the central Indian Ocean, west of Diego Garcia. After strengthening into a moderate tropical storm on 18 December, the storm rapidly intensified while moving westward, taking advantage of favorable atmospheric conditions. Within 18 hours of being named, Bondo intensified to tropical cyclone status, or the equivalent of a minimal hurricane. The Météo-France office on Réunion (MFR) estimated peak 10-minute sustained winds of 205 km/h (125 mph), although the American-based Joint Typhoon Warning Center estimated stronger 1-minute winds of 250 km/h (155 mph). While near peak intensity, Bondo passed just south of Agaléga island, before weakening slightly and moving through the Farquhar Group of islands belonging to the Seychelles, becoming the strongest cyclone to affect that island group in decades. Bondo turned southwestward, and after brushing the northern coast of Madagascar, the cyclone made landfall near Mahajanga on 25 December. The storm continued southward, and was last tracked by the MFR on 28 December.
This timeline documents all of the events of the 2009–10 South-West Indian Ocean cyclone season which is the period that tropical cyclones formed in the Indian Ocean. Within the Indian Ocean most tropical cyclones form within the cyclone season which began on November 1 and will end on April 30. The scope of this article is limited to tropical cyclones that form in the Indian Ocean 30°E and 90°E to the south of the equator. When a zone of disturbed weather form or moves into the South-West Indian Ocean it is assigned a number and monitored by Météo-France who run the Regional Specialized Meteorological Center (RSMC) on Réunion Island. Should a tropical disturbance intensify and become a moderate tropical storm the two sub-regional tropical cyclone Advisory Centres in Mauritius and Madagascar in conjunction with RSMC La Réunion. The United States Joint Typhoon Warning Center (JTWC) also issue warnings on tropical cyclones in this region assigning a number with an "S" suffix. When monitoring a tropical cyclone the Joint Typhoon Warning Center will assess the cyclones intensity on the Saffir–Simpson hurricane scale whilst RSMC La Réunion, Mauritius and Madagascar use the Southwest Indian Ocean Tropical Cyclone Intensity Scale to assess a tropical cyclones intensity.
The 2012–13 South-West Indian Ocean cyclone season was a slightly above average event in tropical cyclone formation in the Southern hemisphere tropical cyclone year starting on July 1, 2012, and ending on June 30, 2013. Within this basin, tropical and subtropical disturbances are officially monitored by the Regional Specialised Meteorological Centre on Réunion island, while the Mauritius and Madagascar weather services assign names to significant tropical and subtropical disturbances. The first tropical disturbance of the season developed on October 12 and rapidly developed into the earliest known intense tropical cyclone on record during October 14.
Tropical Cyclone Haruna was a deadly storm that produced widespread flooding and a disease outbreak in southwestern Madagascar. The ninth system of the season, Haruna developed in the Mozambique Channel in the middle of February 2013 between Mozambique and southwestern Madagascar. Initially moving northward over Mozambique, the disturbance later moved slowly southward, gradually strengthening into the eighth named storm of the season and later into an intense tropical cyclone. The Météo-France office in Réunion (MFR) – the official Regional Specialized Meteorological Center in the basin – estimated the cyclone attained peak 10 minute sustained winds of 150 km/h (95 mph). Haruna made landfall near Morombe in southwestern Madagascar on February 22. It weakened significantly while crossing the country, and MFR discontinued advisories on February 24 after the storm had emerged into the Indian Ocean.
Very Intense Tropical Cyclone Hellen of March 2014 was one of the most powerful tropical cyclones in the Mozambique Channel on record, as well as the most intense of the 2013–14 South-West Indian Ocean cyclone season. Hellen formed on March 26 in the northern portion of the channel, and the storm brought rainfall to coastal Mozambique while in its formative stages. While moving southeastward, it developed an organized area of convection over the center of circulation. Warm waters allowed Hellen to rapidly intensify while passing south of the Comoros, with a well-defined eye forming in the middle of the thunderstorms. The cyclone attained peak intensity March 30, with maximum sustained winds estimated 230 km/h (145 mph) according to the Regional Specialized Meteorological Center, Météo-France in La Réunion. Subsequently, Hellen weakened quickly due to dry air and land interaction with Madagascar, and the storm's eye dissipated. On March 31, the storm made landfall in northwestern Madagascar as a weakened cyclone, despite previous forecasts for the center to remain over water. By April 1, Hellen was no longer a tropical cyclone after most of the convection dissipated. The remnants turned to the west, moving over Mozambique without redeveloping, later dissipating on April 5.
The 2016–17 South-West Indian Ocean cyclone season was a below-average season, with five tropical storms, three of which intensified into tropical cyclones. It officially began on November 15, 2016, and ended on April 30, 2017, with the exception for Mauritius and the Seychelles, for which it ended on May 15, 2017. These dates conventionally delimit the period of each year when most tropical and subtropical cyclones form in the basin, which is west of 90°E and south of the Equator. Tropical and subtropical cyclones in this basin were monitored by the Regional Specialised Meteorological Centre in Réunion, though the Joint Typhoon Warning Center issued unofficial advisories.
The 2021 Pacific typhoon season was the second consecutive season to have below average tropical cyclone activity, with twenty-two named storms, and was the least active since 2011. Nine became typhoons, and five of those intensified into super typhoons. This low activity was caused by a strong La Niña that had persisted from the previous year. The season's first named storm, Dujuan, developed on February 16, while the last named storm, Rai, dissipated on December 21. The season's first typhoon, Surigae, reached typhoon status on April 16. It became the first super typhoon of the year on the next day, also becoming the strongest tropical cyclone in 2021. Surigae was also the most powerful tropical cyclone on record in the Northern Hemisphere for the month of April. Typhoons In-fa and Rai are responsible for more than half of the total damage this season, adding up to a combined total of $2.02 billion.
Tropical Cyclone Ava was a strong tropical cyclone that brought devastating impacts to parts of eastern Madagascar in January 2018. The first tropical depression, first named storm, and first tropical cyclone of the 2017–18 South-West Indian Ocean cyclone season, Ava formed as a weak area of disturbed weather well northeast of St. Brandon on December 30. Monitored by Météo-France La Réunion (MFR), the disturbance drifted southwest, before intensifying to a moderate tropical storm on January 2. Ava drifted south afterwards with little change in strength; then among favorable conditions near the coast of Madagascar Ava rapidly intensified to tropical cyclone intensity by early on January 5 shortly before making landfall in eastern Madagascar. After landfall, Ava pummeled the region with rainfall and flooding as it weakens into a moderate tropical storm. Ava exited the landmass on January 7 and became post-tropical southeast of southern Madagascar on January 8, slowly drifting southwards as a vigorous low before dissipating a day later.
Typhoon Faxai, known in Japan as Reiwa 1 Bōsō Peninsula Typhoon, was the first typhoon to strike the Kantō region since Mindulle in 2016, and the strongest typhoon to hit the region since Ma-on in 2004. It was also the worst to hit the region since Talas in 2011, until the region was hit by the more destructive Typhoon Hagibis less than a month later. Forming as the fifteenth named storm of the 2019 Pacific typhoon season, the precursor to Faxai was first noted as a weak tropical depression to the east of the International Dateline on August 29. The depression then entered the West Pacific basin on August 30. After moving in a general westward direction, the system strengthened into a named tropical storm by September 5. Faxai then strengthened into the sixth typhoon of the season the next day. Two days later, Faxai reached its peak strength as a Category 4 typhoon just before making landfall in mainland Japan. Turning northeastward, Faxai rapidly weakened and became extratropical on September 10.
The 2020–21 South-West Indian Ocean cyclone season was an above-average season which produced 12 named storms, with 7 strengthening into tropical cyclones. The season started with the formation of Cyclone Alicia in the extreme northeast section of the basin on 12 November 2020, just before the official start of the season, which marked the third season in a row in which a tropical cyclone formed before the official start of the season. It officially began on 15 November 2020, and ended with the dissipation of Cyclone Jobo on 24 April, 6 days before the official end on 30 April 2021, with the exception of Mauritius and the Seychelles, which officially ended on 15 May 2021. These dates conventionally delimit the period of each year when most tropical and subtropical cyclones form in the basin, which is west of 90°E and south of the Equator. Tropical and subtropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion and unofficially by the Joint Typhoon Warning Center.
Tropical Cyclone Guambe was the third tropical cyclone to make landfall in the country of Mozambique since December 2020, following Cyclone Eloise and Tropical Storm Chalane. The eleventh tropical depression, eighth named storm, and the fourth tropical cyclone of the 2020–21 South-West Indian Ocean cyclone season, Guambe originated from a tropical disturbance in the Mozambique Channel on 10 February. Two days later, the system developed into a subtropical depression that made landfall in Mozambique. The storm proceeded to make a clockwise loop over the country for the next several days, while dumping prolific amounts of rainfall in the region, before re-emerging into the Mozambique Channel on 16 February. Soon afterward, the system strengthened into a moderate tropical storm and was named Guambe. A couple of days later, Guambe underwent rapid intensification, reaching tropical cyclone status on 19 February, and peaking as a Category 2-equivalent tropical cyclone shortly afterward. Afterward, Guambe underwent an eyewall replacement cycle and weakened back into a severe tropical storm on 20 February. Afterward, Guambe transitioned into an extratropical storm on 22 February. On the next day, Guambe was absorbed into another extratropical cyclone.
The 2021–22 South-West Indian Ocean cyclone season featured the record latest start for the first system to develop. Despite the late start, it was an above-average season that produced 12 named storms, with five becoming tropical cyclones. The season began on 15 November 2021, and ended on 30 April 2022, with the exception for Mauritius and the Seychelles, for which it ended on 15 May 2022. These dates conventionally delimit the period of each year when most tropical and subtropical cyclones form in the basin, which is west of 90°E and south of the Equator. However, tropical cyclones that form at any time between July 1st, 2021 and June 30th, 2022 will count towards the season total. Tropical and subtropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion and unofficially by the Joint Typhoon Warning Center.
Severe Tropical Storm Ana was a deadly tropical cyclone that affected the African nations of Madagascar, Malawi and Mozambique and was the third-deadliest tropical cyclone in 2022, after the Western Pacific Tropical Storm Megi and Atlantic Hurricane Ian. The first named storm of the 2021–22 South-West Indian Ocean cyclone season, Ana developed from an area of convection that was designated as Invest 93S northeast of Madagascar.
Tropical Cyclone Gombe was a strong tropical cyclone that affected Mozambique. It became the first storm to make a major landfall in Nampula Province in Mozambique since Cyclone Jokwe in 2008. The eighth tropical storm, fourth tropical cyclone and fourth intense tropical cyclone of the 2021–22 South-West Indian Ocean cyclone season, Gombe originated from a tropical disturbance located off the coast of Madagascar. This area of convection was designated by the Joint Typhoon Warning Center as Invest 97S on 6 March. The next day, it began to slowly move westward and executed a loop as it became more organized, which prompted Météo-France Reunion (MFR) to note the system as Zone of Disturbed Weather 09. The system became a depression on 9 March, and became a moderate tropical storm the same day. Soon after being named, Gombe made landfall in Madagascar, and entered in the Mozambique Channel the next day. The storm continued its westward motion while slowly intensifying, and was upgraded to a Tropical Cyclone by the MFR on 10 March. Closing in on Nampula Province, the storm underwent rapid intensification, and was upgraded to the fourth Intense Tropical Cyclone of the year and reached its peak intensity on 11 march, with maximum 10-minute sustained winds of 165 km/h (105 mph), maximum 1-minute sustained winds of 185 km/h (115 mph), and a minimum central pressure of 960 hectopascals (28 inHg). The storm proceeded to make landfall, and quickly lost its convection over land. On 12 March, Gombe degenerated into a remnant low overland. However, the system subsequently turned southeastward and reemerged over water, before briefly regenerating into a tropical depression on 17 March. Gombe dissipated later that day.
The 2022–23 South-West Indian Ocean cyclone season was one of the deadliest South-West Indian cyclone seasons on record, mostly due to Cyclone Freddy. It officially began on 15 November 2022, and ended on 30 April 2023, with the exception for Mauritius and the Seychelles, for which it ended on 15 May 2023. These dates conventionally delimit the period of each year when most tropical and subtropical cyclones form in the basin, which is west of 90°E and south of the Equator. However, tropical cyclones can form year-round, and all tropical cyclones that form between 1 July 2022 and 30 June 2023 will be part of the season. Tropical and subtropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion and unofficially by the Joint Typhoon Warning Center. The season was average in terms of the number of systems that formed, with nine systems becoming at least moderate tropical storms, and six reaching tropical cyclone strength. Activity began early, with the first two systems developing in September and October, and ended late with Fabien in May.
The 2022–23 Australian region cyclone season was the fourth consecutive season to have below-average activity in terms of named storms. The season officially started on 1 November 2022 and finished on 30 April 2023, however, a tropical cyclone could form at any time between 1 July 2022 and 30 June 2023 and would count towards the season total, as Tropical Cyclone 01U proved in July 26. During the season, tropical cyclones were officially monitored by one of the three tropical cyclone warning centres (TCWCs) for the region which are operated by the Australian Bureau of Meteorology, National Weather Service of Papua New Guinea and the Indonesian Agency for Meteorology, Climatology and Geophysics. The United States Joint Typhoon Warning Center (JTWC) and other national meteorological services including Météo-France and the Fiji Meteorological Service also monitored the basin during the season.
Tropical Cyclone Cheneso was a strong tropical cyclone that affected Madagascar in January 2023. The fourth tropical storm and fifth tropical cyclone of the 2022–23 South-West Indian Ocean cyclone season, Cheneso developed out of a zone of disturbed weather status which was first monitored at RSMC La Réunion on 17 January. Despite convection wrapping into the curved band pattern, the system formed into a tropical depression on 18 January. The depression strengthened into Severe Tropical Storm Cheneso on the following day. Cheneso made landfall over northern Madagascar and weakened into an inland depression, before emerging into the Mozambique Channel. Cheneso later strengthened into a tropical cyclone on 25 January. The system continued moving southeast, before transitioning into a post–tropical depression on 29 January.
Very Intense Tropical Cyclone Freddy, also known as Severe Tropical Cyclone Freddy, was an exceptionally long-lived, powerful, and deadly tropical cyclone that traversed the southern Indian Ocean for more than five weeks in February and March 2023. Freddy was the longest-lasting tropical cyclone ever recorded worldwide, and produced the most accumulated cyclone energy—a metric used to measure the total energy generated by tropical cyclones—of any individual cyclone on record globally. Additionally, it is the third-deadliest tropical cyclone recorded in the Southern Hemisphere, only behind 2019's Cyclone Idai and the 1973 Flores cyclone.
The 2023–24 Australian region cyclone season was the fifth consecutive season to have below-average activity in terms of named storms. Despite this, it was the second in a row to have at least five severe tropical cyclones, including Australia's wettest tropical cyclone on record. The season officially started on 1 November 2023 and ended on 30 April 2024, however, a tropical cyclone could form at any time between 1 July 2023 and 30 June 2024 and would count towards the season total. During the season, tropical cyclones were officially monitored by one of the three tropical cyclone warning centres (TCWCs) for the region which are operated by the Australian Bureau of Meteorology, National Weather Service of Papua New Guinea and the Indonesian Agency for Meteorology, Climatology and Geophysics. The United States Joint Typhoon Warning Center (JTWC) and other national meteorological services including Météo-France and the Fiji Meteorological Service will also monitor the basin during the season.
The 2023–24 South-West Indian Ocean cyclone season was an above-average season, including ten named storms, six tropical cyclones and two intense tropical cyclones. Despite its moderate activity, it was the least deadly and destructive season in three years. It is the current event of the annual cycle of tropical and subtropical cyclogenesis. It began on 15 November 2023, and ended on 30 April 2024, with the exception for Mauritius and the Seychelles, where it ended on 15 May 2024. These dates conventionally delimit the period of each year when most tropical and subtropical cyclones form in the basin, which is west of 90°E and south of the Equator. However, tropical cyclones can form year-round, and all tropical cyclones that formed between 1 July 2023 and 30 June 2024 would be part of the season. Tropical and subtropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion and unofficially by the Joint Typhoon Warning Center.