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Cyclone Nadia

South-West Indian tropical cyclone in 1994

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Through Atmospheric circulation

Damage was heaviest in Mozambique, estimated at $20 million (1994 USD). Cyclone Nadia severely affected four provinces in the country, primarily Nampula Province where it moved ashore. There, 85% of the houses were destroyed, and across its path, the cyclone left 1.5 million people homeless. High winds caused widespread power outages, left areas without water, and significantly damaged crops, notably the cashew crop. The storm struck before the harvest, and lack of food resulted in 300 deaths in the months after the storm. Across Mozambique, Nadia directly caused 240 deaths and injured thousands. Effects spread as far inland as Malawi.

Meteorological history

A disturbance in the Indian Ocean Intertropical Convergence Zone became evident southeast of the Chagos Archipelago on 16 March after two cyclones moved away from the region. Based on analysis from Météo-France, the system slowly organized while moving westward, its movement influenced by a subtropical ridge to the south. On 17 March, the JTWC also began tracking the system. Due to cool, dry air, the system initially did not intensify, although its passage over warmer sea surface temperatures on 19 March allowed for strengthening. That same day, MF classified the disturbance as Tropical Storm Nadia after rainbands developed. A day later, the JTWC designated Nadia as Tropical Cyclone 23S.

After becoming a tropical storm, Nadia quickly intensified, developing a central dense overcast and later an eye. With minimal wind shear, the storm strengthened into a tropical cyclone early on 21 March. That day, the JTWC estimated winds of 120 km/h (75 mph 1-minute sustained), or the equivalent of a minimal hurricane, and later that day, MF upgraded Nadia into an intense tropical cyclone. While the cyclone was approaching northern Madagascar on 22 March, MF estimated that Nadia attained maximum sustained winds of 175 km/h (110 mph (10 minute sustained)). At around the same time, the JTWC estimated winds of about 220 km/h (140 mph (1-minute sustained)). While at peak intensity, Nadia had well-defined outflow and an eye no larger than 30 km (19 mi). At about 0100 UTC on 23 March, Nadia made landfall on northern Madagascar near Vohemar, having weakened slightly from its peak.

While located over Madagascar, Nadia weakened into a tropical storm due to the mountainous terrain. With warm temperatures, the storm re-intensified slightly after entering the Mozambique Channel, and it passed about 100 km (62 mi) south of Mayotte at 1900 UTC on 23 March. At 1700 UTC the next day, Nadia made its second landfall on Mozambique, about halfway between Nacala and Moçambique. Shortly thereafter, the JTWC discontinued advisories. Despite moving further inland, Nadia retained a well-organized circulation and convection. The storm turned to the south and re-emerged into the Mozambique Channel late on 26 March near the mouth of the Zambezi River. Nadia gradually re-intensified while curving to the southeast, and it re-intensified into a tropical storm on 28 March, the same day the JTWC resumed issuing advisories. The storm strengthened to reach a secondary peak intensity of 85 km/h (50 mph (10 minute sustained)), according to MF. After reaching a position about halfway between Mozambique and Madagascar, Nadia turned to the southwest on 1 April and lost its remaining convection. The JTWC and MF discontinued advisories that day, and the circulation dissipated a day later.

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