 Despite predictions for no further intensification , Kesiny redeveloped convection late on May 8 that organized into a central dense overcast . By early on May 9 , another eye had developed , and the storm quickly intensified into a tropical cyclone , according to MFR . This occurred despite little change in atmospheric conditions , although outflow had improved . Later on May 9 , Kesiny struck northeastern Madagascar about 60 km ( 37 mi ) southeast of Antsiranana , with peak winds of 130 km / h ( 81 mph ) . This made it the first known tropical cyclone on record to make landfall in the month in the basin . While crossing northern Madagascar , the eye quickly dissipated , and the winds decreased . Although re @-@ intensification was expected over the Mozambique Channel , Kesiny remained weak while turning toward the south . On May 10 , the storm weakened to a tropical depression , and subsequently it made a second landfall about 75 km ( 47 mi ) northeast of Mahajanga . Kesiny dissipated on May 11 while inland . 
