What was the first storm to develop in the 1999–2000 South-West Indian Ocean tropical cyclone season?
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The 1999–2000 South-West Indian Ocean tropical cyclone season was the first on record in which two storms – Leon–Eline and Hudah – struck Mozambique at tropical cyclone intensity, or with maximum sustained winds of at least 120 km/h (75 mph). The most notable storm of the season was Eline, which was the longest-lasting storm on record in the basin. It lasted for 29 days while traversing the southern Indian Ocean, making the strongest landfall in decades along eastern Madagascar in late February. The storm was the first in a series of three storms that struck the country in early 2000, along with Gloria in March and Hudah in April. Collectively, the three storms killed at least 316 people. The season started on November 1, 1999, and ended for most of the basin on April 30, 2000; for Mauritius and the Seychelles, the season continued until May 15. These dates conventionally delimit the period of each year when most tropical cyclones form in the basin;
1999–2000 South-West Indian Ocean cyclone season
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The same monsoon trough that spawned Connie also produced an area of convection southeast of Diego Garcia on January 28. The circulation slowly organized, and the MFR classified it as a tropical disturbance on January 30. A nearby trough steered the system southeastward initially and later to the southwest. On January 31, the system became a tropical depression, and later Moderate Tropical Storm Damienne the next day, reaching peak winds of 65 km/h (40 mph). Also on February 1, the JTWC initiated warnings on Tropical Cyclone 10S, which estimated 1‑minute winds of 95 km/h (60 mph). Increased wind shear removed the convection on February 2, causing marked weakening, and prompting the JTWC to discontinue advisories that day. This was despite forecasts of strengthening to near tropical cyclone status. As a weak tropical disturbance, Damienne turned to a rapid westward motion, passing north of Rodrigues and Tromelin. The circulation dissipated on February 7 off the northeast coast of Madagascar.
On February 1, a low-pressure area formed within the monsoon trough to the south of Indonesia, which would eventually become Tropical Cyclone Leon in the Australian basin, as well as Tropical Cyclone 11S according to JTWC. The storm tracked westward across much of the Indian Ocean, fluctuating in strength due to changes in the atmosphere. After crossing 90° E, the MFR began tracking the system as Tropical Storm Eline on February 8. The storm continued westward across the Indian Ocean and intensified greatly as it approached the east coast of Madagascar. Late on February 17, Eline made landfall near Mahanoro with 10‑minute winds of 165 km/h (105 mph), making it the strongest storm to hit the country in several decades. The storm rapidly weakened over land, but restrengthened in the Mozambique Channel to reach peak 10‑minute winds of 185 km/h (115 mph). On February 22, Eline made landfall about 80 km (50 mi) south of Beira, Mozambique near peak intensity and quickly weakened over land. The well-defined circulation moved across southern African, finally dissipating over eastern Namibia on February 29. Throughout its duration, Leon–Eline lasted 29 days, a record longevity for a storm in the south-west Indian Ocean. The track was over 11,000 km (6,800 mi), or about 25% of the Earth's circumference.
1999–2000 South-West Indian Ocean cyclone season
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The 2000–01 South-West Indian Ocean cyclone season was a fairly quiet season with only five named storms, although there was an additional unnamed tropical storm and two subtropical cyclones with gale-force winds. It started early, with a tropical disturbance forming on August 1 – the first day of the cyclone year. However, the first named storm, Ando, was not named until January 2, which at the time was the 4th latest on record. Ando would become the most intense cyclone of the year, reaching peak winds of 195 km/h (120 mph) according to the Météo-France office (MFR) on Réunion, the official Regional Specialized Meteorological Center for the basin. The agency tracked storms south of the Equator and west of 90°E to the east coast of Africa.
2000–01 South-West Indian Ocean cyclone season
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The 1984–85 South-West Indian Ocean cyclone season was an average cyclone season. Tropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion. The first storm formed in mid-November, though it was not officially named. A few days later, the first official storm of the year (Anety) formed. In December, one storm formed. During January 1985, two tropical cyclones formed towards the end of the month. Three more systems developed in a short period of time in early to mid-February. After nearly two more months of inactivity, an unusually powerful late season storm developed (Helisaonina) in mid-April, which was the strongest storm of the year. While a number of storms during the season reached severe tropical storm status, only one of those intensified further. Even though two tropical cyclones this year made landfall, no known damage was recorded.
1984–85 South-West Indian Ocean cyclone season
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The 1995–96 South-West Indian Ocean cyclone season was a moderately active season that included Cyclone Bonita, which was the first known tropical cyclone to cross from the southern Indian Ocean into the southern Atlantic Ocean. Tropical activity lasted for about six months from the middle of November 1995 to early May 1996. The first storm, Intense Tropical Cyclone Agnielle, formed in the adjacent Australian basin on November 16 and later reached peak winds in the south-west Indian Ocean. The next named storm after Agnielle was Bonita, which formed in early January and killed 42 people. The basin was most active in February, with two tropical cyclones, or the equivalent of a minimal hurricane, as well as a severe tropical storm. The first of these three was Doloresse, which killed 67 people due to a shipwreck in the Comoros. The next storm was Cyclone Edwige, which caused heavy crop damage on Mauritius before looping along the east coast of Madagascar. In March, both Cyclone Flossy and Tropical Storm Guylianne passed near the Mascarene Islands, producing heavy rainfall and gusty winds.
1995–96 South-West Indian Ocean cyclone season
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The season began later than usual, the third consecutive one to do so. There were no indications of tropical cyclogenesis before the middle of December, putting the season among the latest 20% since 1967 in terms of seasons' first storms. On December 26, the MFR utilized the QuikSCAT satellite for the first time in the basin to assess a storm's intensity. During the season, 14 tropical disturbances formed, which is near average, and they tended to last longer than normal. Eleven of these disturbances became tropical depressions, of which nine attained gale force winds and were named. In addition, four storms reached tropical cyclone intensity, or 10‑minute sustained winds of 120 km/h (75 mph). The 9 named storms and 4 tropical cyclones is also the basin average for each category in a given year. There were 61 days in which a storm was active, greater than the median of 48 and more than double than the previous season. In general, storms formed south of 10° S, with the exception of the first storm Astride, and most storms generally tracked east to west due to a strong ridge east of Madagascar.
1999–2000 South-West Indian Ocean cyclone season
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In August, a tropical depression developed in the south-west Indian Ocean for the first time 27 years, and a month later, a rare September tropical disturbance formed. The first named storm, Antoinette, was the first of several to originate in the neighboring Australian basin, or east of 90° E; the subsequent two named storms also formed in the Australian region. In early December, Cyclone Daniella likely developed out of the remnants of previous Tropical Storm Chantelle. After reaching peak 10–minute winds of 185 km/h (115 mph), Daniella weakened and passed just southwest of Mauritius; there, the storm left heavy crop damage and indirectly caused three deaths. In early January, Tropical Storm Fabriola was the first in a succession of three storms to move over Madagascar. The next – Cyclone Gretelle – killed 152 people when it struck southeastern Madagascar. Between January and February, Cyclone Pancho-Helinda lasted about 20 days between both the Australian and south-west Indian basins. Also in February, Tropical Storm Josie killed 36 people in western Madagascar after causing severe flooding. The final named storm was Tropical Storm Lisette, which dissipated on March 3 after striking Mozambique, killing three people. Despite the early end to the named storms, there were two additional disturbances, one of which became the first July tropical depression in 25 years.
1996–97 South-West Indian Ocean cyclone season
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The 1997–98 South-West Indian Ocean cyclone season was fairly quiet and had the latest start in 30 years. The first tropical disturbance originated on January 16, although the first named storm, Anacelle, was not upgraded until February 8, a record late start. The last storm to dissipate was an unusually late tropical depression in late July. Many of the storms suffered from the effects of wind shear, which contributed to there being only one tropical cyclone – equivalent to a minimal hurricane. The season also occurred during a powerful El Niño.
1997–98 South-West Indian Ocean cyclone season
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Aside from a tropical disturbance in August, the season began later than usual, the fourth consecutive season to do so. At the time it had the 4th latest start on record for the first named storm. Only about 20% of seasons have their first storm form after the middle of December, and the first named storm of this season, Ando, did not become a tropical storm until early January. However, January was active with three tropical cyclones, two of which became intense tropical cyclones, due to the active phase of the Madden–Julian oscillation (MJO). February returned to a period of inactivity, and generally there was minimal convection across the basin due to unusually dry air. This was spread by a powerful and persistent ridge that extended eastward from Madagascar, as well as an inactive phase of the MJO. Drought conditions occurred on Réunion due to the lack of rainfall. After three weeks of no tropical cyclones developing worldwide, an event unseen since 1995, the tropics became active again in early April.
2000–01 South-West Indian Ocean cyclone season
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The 1992–93 South-West Indian Ocean cyclone season lasted longer than normal, with the first storm Aviona forming on September 27 and the final storm Konita not dissipating until May 7. It was an above-average season, with four tropical cyclones – the equivalent of a minimal hurricane – along with six tropical storms, one subtropical depression, and several depressions including one that was named. The basin is defined as the area west of 90°E and south of the Equator in the Indian Ocean, which includes the waters around Madagascar westward to the east coast of Africa. Tropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion (MFR), as well as by the Joint Typhoon Warning Center (JTWC).
1992–93 South-West Indian Ocean cyclone season
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The 2013–14 South-West Indian Ocean cyclone season was an above average event in tropical cyclone formation. The season officially began on July 1, 2013, though the first tropical system designated by Météo-France was a short-lived tropical disturbance that developed on July 8. However, the first named storm was Cyclone Amara in December. Bruce was the first very intense tropical cyclone since Edzani in 2010, which originated from the Australian region. The strongest system of the cyclone season was Hellen, also one of the most intense tropical cyclones over the Mozambique Channel. The season officially ended on June 30, 2014
2013–14 South-West Indian Ocean cyclone season
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Despite the destructive nature of the season, it began later than usual. Cyclone Astride originated toward the end of December, bringing rainfall and gusty winds to northern Madagascar while in the region. In January, cyclones Babiola and Connie both formed east of Madagascar and took southerly tracks. Connie passed near Réunion island, producing of rainfall in the mountainous peaks and killing two people. Eline, the longest lasting storm of the season, struck Mozambique while the country was experiencing its worst flooding in 50 years, collectively causing around 700 deaths and about $500 million in damage. The storm also killed 12 people in Zimbabwe and 21 in South Africa. Just two weeks after Eline struck Madagascar, Tropical Storm Gloria affected the same general region, bringing additional deaths and damage. Cyclone Hudah in April was the strongest storm of the season, reaching peak 10‑minute winds of 220 km/h (140 mph). It caused three deaths in Mozambique, although its effects were worse in Madagascar, where there were 111 deaths. The final storm of the season was Tropical Storm Innocente, which dissipated on April 24. In addition to the named storms, there were four unnamed tropical disturbances or storms, as well as one subtropical cyclone that formed in the southern Mozambique Channel.
1999–2000 South-West Indian Ocean cyclone season
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As a developing disturbance, Gloria produced winds approaching gale-force on St. Brandon. Similar conditions were reported on Tromelin. When Gloria struck Madagascar, it produced sustained winds of 72 km/h (45 mph) at Antalaha, about 70 km (45 mi) south of Sambava. The storm brought heavy rainfall, with Mananjary reporting a two‑day total of . The rains from Gloria occurred less than two weeks after Cyclone Leon–Eline struck the country, bringing additional flooding, landslides, and damage. In Sambava, near where Gloria moved ashore, the storm killed 18 people, destroyed hundreds of homes, and damaged a road connecting the area to the capital of Madagascar, Antananarivo. Farther inland, the cyclone killed 40 people at Andapa. Overall, Gloria killed at least 66 people, although the exact toll was initially unknown due to disrupted communications. Before Gloria emerged into the Mozambique Channel, various news outlets noted the potential for the storm to affect storm-ravaged Mozambique. However, minimal rainfall accompanied Gloria's final landfall. The rains were enough to delay flights for a day, which were transporting relief aid following Eline's devastating landfall in Mozambique.
A tropical low formed in the Australian basin on March 24, moving westward due to a strong subtropical ridge to the south. Despite having intensified enough, the Bureau of Meteorology did not name the system, and on March 25 the system crossed into the South-West Indian Ocean, whereupon it was named Hudah. An eye formed, and the storm intensified into a tropical cyclone on March 27 well to the southeast of Diego Garcia. The structure fluctuated due to dry air, although Hudah was able to intensify steadily on March 31 after conditions became more favorable. The next day, the MFR upgraded it to a very intense tropical cyclone, estimating peak 10‑minute winds of 225 km/h (140 mph). By contrast, the JTWC estimated 1‑minute winds of 235 km/h (145 mph). Cyclone Hudah maintained peak winds until making landfall just southeast of Antalaha, Madagascar on April 2. It weakened greatly over land, but like Eline it re-intensified over the Mozambique Channel. It re-attained tropical cyclone status on April 5 and reached 10‑minute winds of 160 km/h (100 mph) by the time it made landfall on Mozambique near Pebane, Mozambique on April 8. It dissipated by the next day.
1999–2000 South-West Indian Ocean cyclone season