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.
Tropical activity continued through April and May, with two tropical cyclones in the former month. In early April, Tropical Cyclone Hansella moved over the island of Rodrigues, dropping more rainfall in 24 hours than the average monthly total. Later, Itelle became a rare April intense tropical cyclone, but weakened before it approached St. Brandon island. The final storm of the season, Jenna, formed in the Australian region, briefly intensified into a minimal tropical storm in the south-west Indian Ocean, and proceeded to exit the basin on May 4 to end the season. In addition to the named storms, several tropical depressions were tracked, one of which in December dropped heavy rainfall on Réunion. __TOC__
Seasonal summary
During the season, the Météo-France office (MFR) on Réunion island issued warnings in tropical cyclones within the basin. The agency estimated intensity through the Dvorak technique, and warned on tropical cyclones in the region from the coast of Africa to 90° E, south of the equator. The Joint Typhoon Warning Center (JTWC), which is a joint United States Navy – United States Air Force task force, also issued tropical cyclone warnings for the southwestern Indian Ocean.
The season was fairly active with ten tropical storms, one greater than average, although most storms were short-lived. Six of the storms reached tropical cyclone status, or maximum sustained winds of at least , which is two more than average. Most cyclones dissipated within the tropics, in contrast to the norm of storms accelerating into higher latitudes. Throughout the season there were 82 days in which there was tropical activity. Based on a list contributed by the nation of Seychelles, the storms were named in sequential order, starting with Agnielle. The rest of the names on the list were Ketty, Lucia, Molly, Nadege, Odette, Paquerette, Rolina, Sylvianne, Talla, Vivienne, Walya, and Yoline.
In addition to the named storms, the MFR tracked 11 tropical depressions or disturbances that did not intensify into a tropical storm. The agency did not issue any bulletins on eight of them. Of the remaining three, two formed in late December, and the other formed in mid-February. Tropical Depression B2, the longest lasting of the depressions, formed after a month of activity. An area of convection developed in the Mozambique Channel, and the MFR believed it to be connected to the depression that formed on December 28 east of Madagascar. With a ridge to the east, the system tracked southward, but failed to intensify due to strong wind shear. While passing west of Réunion, the depression dropped heavy rainfall, totaling along the northern coast and about twice that amount in the mountainous interior. On December 31, the depression dissipated to the southwest of Réunion. On February 10, the JTWC tracked Tropical Cyclone 12S into the basin as a weakening tropical depression, which quickly dissipated. A few days later, the JTWC also tracked Tropical Cyclone 15S from February 14–17, which briefly intensified into a minimal tropical storm in the eastern portion of the basin.
Systems Intense Tropical Cyclone Daryl–Agnielle
In the middle of November 1995, the Intertropical Convergence Zone (ITCZ) spawned an area of convection to the southwest of the Indonesian island of Sumatra. Located within the Australian region in an area of low wind shear, a tropical low developed west of Sumatra on November 16. It gradually intensified while moving southward, before turning sharply westward on November 18 due to a ridge to the south. That day, the Bureau of Meteorology (BoM) office in Perth upgraded the low to Tropical Cyclone Daryl, or to minimal tropical storm status. Designated Tropical Cyclone 01S by the JTWC, Daryl continued to intensify, and the BoM upgraded it to winds of . The system crossed into the basin on November 19, and was renamed Daryl as Agnielle at that time.
On November 20, the ridge to the south weakened, allowing Agnielle to turn to the southwest. A well-defined eye developed, which persisted for about three days. Late on November 20, Agnielle attained peak 10‑minute sustained winds of , making it an intense tropical cyclone, a rarity for November storms. On November 21, the JTWC estimated peak 1‑minute winds of , the second-strongest storm estimated by the agency in the Indian Ocean, after only Cyclone Fantala. Although the eye briefly became less organized, accompanied by a decrease in winds, Agnielle re-intensified despite moving over colder waters. The ridge to the south rebuilt, forcing the cyclone to slow and turn to the west. Increasing wind shear caused rapid weakening; within 30 hours, the winds decreased from tropical cyclone to tropical depression status on November 25. That day, the JTWC discontinued advisories, although the MFR continued tracking the circulation until Agnielle's dissipation on November 27.
Intense Tropical Cyclone Bonita
As Tropical Depression B2 was dissipating near Réunion, another tropical depression formed east of the Chagos Archipelago on January 3. It moved southwestward, initially without development, but conditions gradually became more favorable. On January 5, the depression strengthened into Tropical Storm Bonita, and three days later reached tropical cyclone status as it developed a well-defined eye. Later that day, Bonita quickly intensified to its 10‑minute peak intensity of , making it the strongest storm of the season. A ridge to the south turned the cyclone more to the west. On January 9, the JTWC estimated Bonita attained peak 1‑minute winds of , and the next day, the cyclone made landfall about north of Foulpointe in eastern Madagascar. Bonita quickly weakened into a tropical storm while crossing the country but re-intensified slightly after reaching the Mozambique Channel on January 12. Late on January 13, Bonita made a second landfall in eastern Mozambique between Pebane and Quelimane. Although the MFR ceased issuing advisories on January 15, the remnants of Bonita continued across Africa, and emerging into the southern Atlantic Ocean on January 19 and dissipating the next day. Bonita was considered by the Zambia Meteorological Department to have been the first tropical cyclone known to have traversed southern Africa from the South-West Indian Ocean to the South Atlantic.
In eastern Madagascar, 24‑hour rainfall totals included at Toamasina, while gusts exceeded on the offshore island of Île Sainte-Marie. Bonita caused widespread flooding of rice crops, as well as heavy infrastructure and crop damage along the northeastern coastline. The cyclone killed 25 people in Madagascar and left 5,000 people homeless. In Mozambique, Bonita dropped heavy rainfall and produced flooding, killing as many as 17 people. Floodwaters destroyed of crops and demolished many buildings, including about 12 schools. The remnants of Bonita dropped the heaviest rainfall in 80 years in eastern Zimbabwe, and heavy rainfall also spread into Zambia.
Severe Tropical Storm Hubert–Coryna
In the Australian basin, the monsoon trough spawned a tropical disturbance near Christmas Island on January 3. With a ridge to the south, the system tracked to the west-southwest, developing into a tropical low on January 6 and being named Hubert the next day by the BoM. It quickly intensified to reach peak 10‑minutes winds of on January 9 to the north of the Cocos Islands, but later that day began weakening due to increasing wind shear. At around 1800 UTC on January 9, Hubert crossed into the south-west Indian Ocean with 10‑minute winds of , and at that time, was renamed the cyclone Coryna. The wind shear quickly tore the convection away from the center, leaving the circulation exposed by January 10. The next day, Coryna weakened to tropical depression status, and on January 12 the circulation dissipated in the central Indian Ocean.
Severe Tropical Storm Doloresse
After about a month in which there were no named storms in the basin, a tropical disturbance formed within the ITCZ to the southwest of Seychelles on February 12. It moved slowly to the southwest with a well-defined center and a broad area of convection. For several days, the system remained weak until reaching more favorable conditions on February 16, and the next day it intensified into Tropical Storm Doloresse. The storm slowed while reaching the western extent of a ridge, drifting for nearly 24 hours about north-northwest of Grande Comore. On February 17, an approaching trough turned Doloresse to the south-southeast, bringing the storm about southwest of Grande Comore; this made it the first cyclone to directly affect the nation since Cyclone Elinah 13 years prior. On February 17, the JTWC estimated peak 1‑minute winds of , and on the next day, the MFR estimated peak 10‑minute winds of . Increasing shear caused Doloresse to rapidly weaken to tropical depression status on February 19. Although the JTWC assessed the storm as continuing to the southeast and striking northwestern Madagascar, the MFR estimated the system turned to a southwest drift and dissipated on February 20.
In the Comoros, Doloresse produced strong wind gusts, damaging crops and houses on Grande Comore. Heavy rainfall caused landslides, and the cyclone caused a shipwreck, killing 67 people on the island of Mohéli. The western periphery of the circulation dropped heavy rainfall in Tanzania.
Tropical Cyclone Edwige
On February 18, a tropical disturbance began forming about southwest of Diego Garcia, becoming a tropical depression the next day. A trough steered the new system to the southeast, but also prevented significant strengthening due to wind shear. Late on February 21, the MFR upgraded the depression to Tropical Storm Edwige, and the next day the JTWC began tracking it as Tropical Cyclone 16S. When the trough weakened, Edwige turned to the south and later southwest, reaching an initial peak of on February 23. That day, increasing wind shear caused the storm to weaken to minimal tropical storm status, and the JTWC briefly discontinued advisories on February 24. The strengthening ridge caused Edwige to accelerate to the west, bringing it south of Rodrigues without any effects on February 24. On the next day, the storm passed north of Mauritius and Réunion, where it produced wind gusts of and , respectively, as well as heavy rainfall. Due to crop damage caused by Edwige, as well as a drought later in the year, Mauritius failed to reach its quota for sugar outputs.