1985–86 South-West Indian Ocean cyclone season
The 1985–86 South-West Indian Ocean cyclone season was the first in which the Météo-France office on Réunion tracked cyclones as far east as 90° E in Indian Ocean, south of the equator. Previously, the agency's area of responsibility was limited to 80° E. It was an active season with twelve named storms, of which five strengthened into tropical cyclone with 10 minute sustained winds of at least 120 km/h. The first named storm was Tropical Storm Alifredy, which originated in the Mozambique Channel in late December and moved across Madagascar. However, the unofficial Joint Typhoon Warning Center tracked a short-lived storm in September.
Most of the activity occurred in 1986, with four storms in January, three of which briefly existed simultaneously on January 10. The first of these three, Tropical Storm Berobia, struck eastern Mozambique. Tropical Storm Costa was a series of three tropical depressions within the same broader system that persisted for 12 days, bringing gusty winds and rainfall to the Mascarene Islands. The strongest storm of the season, Erinesta, formed in late January and struck the tiny Tromelin Island, decimating the native rabbit population. Erinesta later produced of rainfall in the mountainous peaks of Réunion, one of the highest 24‑hour rainfall totals at the time at Cilaos. Two other storms in February - Filomena and Gista - moved southward for their durations and did not significantly impact land. In March, Cyclone Honorinina killed 99 people and caused $150 million in damage when it struck eastern Madagascar. There were two other storms in March, Iarima and Jefotra, the latter of which brushed Rodrigues island with gusty winds. The final two storms of the season, Krisostoma and Lila, entered from the Australian basin in April and May, respectively, with Lila exiting the basin to end the season on May 10.
Seasonal summary
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During the season, the Météo-France office on Réunion island issued warnings in tropical cyclones within the basin. Using satellite imagery from National Oceanic and Atmospheric Administration, 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. In September 1985, their area of responsibility shifted from 80° E to the current 90° E, although lack of satellite imagery along the eastern periphery prevented complete coverage. The World Meteorological Organization would later label the MFR as a Regional Specialized Meteorological Center in 1993. The Joint Typhoon Warning Center, 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's twelve named storms was well above the average of nine, while the five tropical cyclones – storms attaining maximum sustained winds of at least - was average.
The MFR considered the tropical cyclone year to begin on August 1 and continue to July 31 of the following year. By December 1985, water temperatures were cooler than normal across the Indian Ocean. However, the monsoon intensified the following month, allowing for increased tropical cyclogenesis. There were no El Niño conditions by March.
In addition to the storms tracked by the MFR, the JTWC followed a short-lived tropical storm in September. Classified as Tropical Cyclone 01S, the storm developed on September 23 to the east-southeast of Diego Garcia, which is an atoll in the central Indian Ocean. It failed to intensify beyond peak 1 minute winds of 75 km/h, and after passing south of Diego Garcia, the storm dissipated on September 29 south of the Seychelles.
Systems
Moderate Tropical Storm Alifredy
On December 23, a tropical depression formed in the Mozambique Channel, accompanied by spiral rainbands toward the center. That day, the system reached peak winds of 65 km/h, and the Madagascar Meteorological Service named it Alifredy. The storm moved quickly southeastward toward Madagascar. High pressures to the south prevented much development, and Alifredy moved ashore near Morondava in western Madagascar on December 24 at peak intensity. While crossing the island, the storm weakened into a tropical depression. Alifredy emerged into the open Indian Ocean and failed to restrengthen. It became extratropical and turned southeastward, dissipating on December 27 within the westerlies. The JTWC did not track the storm. Alifredy had little impacts on Madagascar; Morombe reported a peak wind gust of.Moderate Tropical Storm Berobia
The Intertropical Convergence Zone spawned a tropical depression in the northern periphery of the Mozambique Channel on January 5, near the Comoros. Initially still located with the ITCZ, the system tracked south-southwestward, although its motion slowed due to a ridge to the south. It passed near Juan de Nova Island on January 6, producing gusts of. By January 7, the system began disassociating itself from the ITCZ and it intensified. That night, the Madagascar Meteorological Service named the depression Berobia, which intensified into a moderate tropical storm the next day. Also on January 8, the JTWC began classifying the storm as Tropical Cyclone 06S. That day, Berobia began moving to the west-northwest, due to the strengthening ridge to the south. On January 9, the storm attained peak winds of 85 km/h according to the MFR; the JTWC estimated a slightly higher 1 minute peak of 95 km/h. Late on January 9, Berobia made landfall about 125 km north of Beira, Mozambique, and it dissipated the next day after entering Zimbabwe. The remnants of Berobia dropped heavy rainfall in northeastern Zimbabwe, with a 24‑hour peak of.Severe Tropical Storm Costa
Tropical Storm Costa was a series of three different tropical depressions within the same broader system that persisted for 12 days east of Madagascar, all given the same name. The first circulation formed on January 7 between the northeast coast of Madagascar and Agaléga. Later that day, the Madagascar Meteorological Service named it Costa, and the JTWC labeled it Tropical Cyclone 05S. It moved eastward and later turned to the southeast, passing near Agaléga before weakening while moving into the ITCZ. Another circulation formed to the east of Costa, and the original circulation dissipated on January 9. The new center moved to the west-southwest toward St. Brandon, although it was disorganized, dissipating on January 11. A third circulation formed on the previous day to the east, becoming a tropical depression with well-organized rainbands. This third system would last the longest, originally moving to the northeast before curving southeastward.On January 12, Costa intensified into a moderate tropical storm. On the next day, the JTWC upgraded it to the equivalent of a minimal hurricane, and the MFR estimated peak winds of 95 km/h. Costa weakened briefly on January 14 while passing about 100 km east of Rodrigues, although it re-attained its former peak on the next day while accelerating southeastward. Costa thereafter weakened rapidly and moved erratically toward the southwest. By January 15, it deteriorated into a minimal tropical storm, and meandered for several days. On January 19, Costa dissipated within the flow of the westerlies.
When Costa formed, it passed near Agaléga, producing wind gusts of. The storm approached St. Brandon twice; on its first passage, Costa produced gusts of during a strong rainband. Later, the storm dropped of rainfall on Rodrigues while producing gusts of.
Tropical Cyclone Delifina
The monsoon was active in early January across the Indian Ocean, spawning what would eventually become Tropical Cyclone Delifina. On January 7, the JTWC classified the system as Tropical Cyclone 04S to the east-southeast Tropical Storm Costa. However, the MFR did not classify it initially due to lack of data. The system had a curved area of convection, and organized enough for MFR to designate it Tropical Storm Delifina on January 10. On the same day, the JTWC upgraded the storm to the equivalent of a minimal hurricane. The storm moved generally southward, after an initial westward movement. Delifina gradually intensified, becoming a tropical cyclone on January 13. By that time, the storm had an eye in the center of deep organized convection. The MFR estimated peak winds of 135 km/h, while the JTWC estimated 1 minute winds of 205 km/h. Subsequently, Delifina weakened as it progressed southward. After turning to the southeast, the deteriorating storm turned sharply northwestward between two ridges. Delifina turned back to the east and dissipated on January 19 at nearly the same longitude where it formed.Intense Tropical Cyclone Erinesta
Satellite imagery indicated that a tropical disturbance formed on January 29 to the southwest of Diego Garcia. It moved westward and slowly organized, becoming a moderate tropical storm on January 31. On the same day, the JTWC classified the storm as Tropical Cyclone 13S, and the Mauritius Meteorological Service named it Erinesta. Its track shifted to a slow west-southwest trajectory while intensifying. The JTWC upgraded the storm to the equivalent of a minimal hurricane on February 1, and the MFR upgraded Erinesta to tropical cyclone status on the next day. On February 4, the cyclone attained peak winds, becoming one of the strongest storms in the basin in several decades. The JTWC estimated peak 1 minute winds of 215 km/h, and the MFR estimated peak winds of 170 km/h. Shortly after Erinesta reached peak intensity, it passed within of Tromelin Island. The storm curved southward due to an approaching trough, briefly threatening to strike Réunion. However, a ridge built behind the trough, bringing the storm between the east coast of Madagascar and the Mascarene Islands. Erinesta gradually weakened, passing west of Réunion as a severe tropical storm on February 7. The storm accelerated to the south-southeast and later became extratropical, dissipating on February 11 within the westerlies.Passing near Tromelin at peak intensity, Erinesta produced peak wind gusts of before damaging the anemometer, with peak winds estimated as high as 250 km/h. The high winds damaged every building and scientific instrument on the island. The passage of the storm killed Tromelin's entire rabbit population. Along the east coast of Madagascar, Erinesta produced wind gusts and 24‑hour rainfall of at Toamasina. Lastly, the cyclone passed west of Réunion, where ten days of precipitation accumulated to at Cilaos, of which fell over 24 hours. The 24‑hour total there was among the highest on record, surpassing even Cyclone Hyacinthe, the wettest storm on record. In one hour, Erinesta dropped of rainfall, which only occurs every two and a half years. This helped replenish aquifer levels, after two years of drought conditions. The rains caused 1 in 10 year flooding in portions of the island, reaching 30 m3/s at Ravine Blanche. While moving past the island, Erinesta produced peak gusts of in the mountainous interior at Plaine des Cafres. The cyclone also produced very high waves along coastal roads, closing them for four days and damaging guard rails.
Moderate Tropical Storm Filomena
In early February, an area of disturbed weather persisted around Diego Garcia, although lack of satellite imagery made it difficult to track the system at first. On February 6, satellite images indicated that a tropical storm formed, given the name Filomena by the Mauritius Meteorological Service. Also on February 6, the JTWC classified it as Tropical Cyclone 14S. Initially the storm moved to the west, although Filomena turned southeastward into an area of low pressure. The storm never intensified beyond winds of 65 km/h according to the MFR. However, the JTWC estimated 1 minute winds of 100 km/h. Filomena gradually weakened as it progress southward. On February 11, the system turned westward and later northwest due to a ridge to the south, having weakened into a tropical depression. Filomena dissipated on the next day.Severe Tropical Storm Gista
On February 18, a circulation formed in the Mozambique Channel, based on satellite imagery. That day, it developed into Moderate Tropical Storm Gista, Early on February 19, the JTWC classified it as Tropical Cyclone 19S. Gista moved generally southward, initially moving to the southeast toward western Madagascar and later curving to the southwest, bringing it within 100 km of the coast. The storm gradually intensified while moving away from the country, reaching peak 10 minute winds of 95 km/h on January 21 about 120 km east of Europa Island. According to the MFR, Gista became extratropical that night, although the JTWC continued tracking it for several more days. According to the JTWC, Gista intensified to the equivalent of a minimal hurricane on February 22 to the southwest of Madagascar, and the next day reached peak 1 minute winds of 160 km/h. Gista accelerated to the southeast and dissipated late on February 24 in the westerlies.While Gista was moving along the west coast of Madagascar, it produced peak wind gusts of at Maintirano. It later produced wind gusts of on Europa Island.
Tropical Cyclone Honorinina
Tropical Storm Honorinina formed on March 9 to the south of Diego Garcia. It moved generally to the west-southwest due to a ridge to the south, gradually intensifying. On March 12, the MFR upgraded Honorinina to tropical cyclone status, which is the equivalent of a minimal hurricane. On the next day, the cyclone attained maximum sustained winds of 150 km/h while in the vicinity of Tromelin Island, although the JTWC estimated peak 1 minute winds of 205 km/h. Honorinina weakened subsequently before making landfall about 40 km north of Toamasina, Madagascar with winds of 135 km/h. The storm weakened further over land, moving southwestward across the country. It emerged into the Mozambique Channel and became extratropical on March 18. Honorinina turned to the southeast, dissipating on March 23.Early in its duration, the storm produced gusty winds along St. Brandon, and it later brought gusts of on Tromelin Island. However, effects were worst in Madagascar, especially in Toamasina near where the storm made landfall. Damage spread along 800 km of the coastline and reached 100 km inland from the landfall point, with many towns severely affected. In Toamasina, the cyclone damaged the main port, the airport, and several warehouses, resulting in $17 million of lost inventory. Thousands of houses were damaged, leaving 83,885 people homeless; a housing program earlier set up after Cyclone Kamisy in 1984 was extended to help storm victims after Honorinina. Nationwide, the cyclone killed 99 people and caused $150 million in damage.