Lably
Skip to content

Tropical Storm Domoina

South-West Indian tropical storm in 1984

  • 10 min read
  • 3 chapters

Related on Lably

Through Indian Ocean

In Mozambique, Domoina dropped heavy rainfall in the capital Maputo that accounted for 40% of the annual total. Floods in the country destroyed over 50 small dams and left widespread crop damage just before the summer harvest. Later, the rains caused the worst flooding in over 20 years in Swaziland, which damaged or destroyed more than 100 bridges. Disrupted transport left areas isolated for several days. In South Africa, rainfall peaked at 950 mm (37 in), which flooded 29 river basins, notably the Pongola River which altered its course after the storm. Flooding caused the Pongolapoort Dam to reach 87% of its capacity; when waters were released to maintain the structural integrity, additional flooding occurred in Mozambique, forcing thousands to evacuate. Throughout the region, Domoina caused widespread flooding that damaged houses, roads, and crops, leaving about $199 million in damage. There were 242 deaths in southeastern Africa.

Meteorological history

In January and February 1984, conditions were favorable for tropical cyclogenesis in the southwest Indian Ocean, including warmer than normal sea surface temperatures and an active monsoon trough. On January 16, a spiral area of convection persisted off the northeast coast of Madagascar, associated with the Intertropical Convergence Zone. That day, it organized enough to warrant a satellite-based Dvorak rating of T2.5, prompting the Réunion Meteorological Service to name it Domoina. Around that time, Météo-France (MFR) estimated winds of about 65 km/h (40 mph). Domoina initially tracked to the west-northwest, passing near Tromelin Island on January 18. Around that time, the storm had begun moving to the southwest, and MFR estimated that it weakened to tropical depression status. On January 19, the Joint Typhoon Warning Center (JTWC) began warning on Domoina, designating it Tropical Cyclone 14S. The same day, MFR again upgraded Domoina into a moderate tropical storm. On January 21, the storm made landfall just south of Tamatave in southeastern Madagascar.

While crossing Madagascar on a westward trajectory, Domonia weakened; JTWC estimated the winds decreased to 55 km/h (35 mph), after earlier estimating winds of 95 km/h (60 mph) before landfall. On January 23, the storm emerged into the Mozambique Channel near Belo, and due to a ridge to the north, it resumed its southwest motion. Domoina executed two small loops off the western coast of Madagascar while progressing generally southwestward. On January 25, MFR estimated that Domonia attained peak 10 minute sustained winds of 95 km/h (60 mph) near Europa Island; this made it a severe tropical storm. Two days later, the JTWC estimated peak 10 minute winds of 100 km/h (60 mph). Early on January 28, Domonia made a second landfall on southeastern Mozambique near peak intensity. It slowly weakened over land while moving across southern Mozambique. The JTWC discontinued advisories on January 29 when the storm was near the border of Mozambique and Swaziland. The next day, Domonia crossed into Swaziland and subsequently into eastern South Africa, weakening into a tropical depression while passing near Durban. At around that time, the system was dissipating, although MFR continued tracking Domonia until February 2, when it dissipated just offshore the east coast of South Africa.

Sign in to keep reading

2 more chapters are free with a Lably account.

More in Earth science