After the disturbance dissipated, a large low pressure area persisted east of Madagascar with several associated circulations. On February 24, Tropical Disturbance D2 passed about 160 km (100 mi) west of Réunion, and continued to the southeast, passing south of Mauritius. Wind shear stripped the convection from the center and caused it to dissipate. Over a nine-day period, the system dropped nearly of rainfall in portions of Réunion, including nearly at Salazie on February 24; at that station, of precipitation fell in just three hours. Gusts reached in some locations. The storm caused flooding and landslides on the island as well as power outages. Rainfall also reached on Mauritius. Residents were generally caught off guard by the storm due to the lack of warnings. Tropical Disturbance D3 also developed before March.