assessed the storm as turning inland again. On February 29, Edwige dissipated just off the coast of Toamasina. The storm dropped of rainfall in Mananjary, with wind gusts of , but damage was limited. Tropical Cyclone Flossy On February 25, a tropical disturbance developed along a cold front about south-southeast of Diego Garcia. With a ridge to the south, the system tracked southwestward and intensified into Tropical Storm Flossy on February 27. That day, the JTWC began issuing advisories on the storm as Tropical Cyclone 17S. The storm quickly developed an eye, intensifying to tropical cyclone status on February 28. That day, the MFR estimated peak 10‑minute winds of 150 km/h (90 mph), while the JTWC estimated peak 1‑minute winds of 215 km/h (130 mph). Late on February 29, Flossy passed about northwest of Rodrigues, producing wind gusts of there. Increased wind shear weakened Flossy, beginning on March 1, although the storm restrengthened slightly on March 2. That day, the cyclone rounded the ridge and turned to the south and southeast, and weakened again due to an approaching cold front. On March 4, Flossy became extratropical after all of the convection was sheared away from the circulation. Two days later, the front absorbed the remnants of Flossy. Moderate Tropical Storm Guylianne The ITCZ spawned a tropical disturbance on March 17 about south of Diego Garcia. Due to ongoing wind shear, the system initially failed to intensify while moving westward. An approaching cold front turned the disturbance southward on March 20 into an area of low wind shear, allowing the convection to increase and for the system to be upgraded to tropical depression status. While the system was moving toward Mauritius on March 22, the depression was upgraded to Tropical Storm Guylianne. Later that night, the storm passed about east of Mauritius, bringing beneficial rainfall. Both MFR and JTWC only estimated peak winds of 65 km/h (40 mph), and Guylianne began weakening on March 23 due to increased wind shear. The storm turned to a southwest drift, dissipating on March 25. Tropical Cyclone Hansella Toward the end of March, the ITCZ was active with several low pressure areas, and an area of convection consolidated south of the Chagos Archipelago in early April. On April 2, a large tropical disturbance formed, and the next day, it was named Hansella despite only being a tropical depression. The system moved westward initially, but curved