▁slowly ▁organized ▁until ▁becoming ▁a ▁tropical ▁storm ▁on ▁March   7 , ▁the ▁same ▁day ▁that ▁the ▁J TW C ▁class ified ▁it ▁as ▁Trop ical ▁Cy clone ▁ 1 7 S . ▁On ▁the ▁next ▁day , ▁the ▁system ▁was ▁named ▁K yl ie ▁as ▁it ▁me ander ed ▁to ▁the ▁north ▁of ▁Maur it ius ▁without ▁further ▁strength ening . ▁The ▁con ve ction ▁organized ▁on ▁March   1 0 ▁into ▁a ▁central ▁dense ▁over cast , ▁and ▁the ▁next ▁day ▁att ained ▁peak ▁wind s ▁of ▁ 8 5   km / h ▁( 5 0   m ph ), ▁according ▁to ▁the ▁M FR . ▁By ▁contrast , ▁the ▁J TW C ▁ass essed ▁K yl ie ▁as ▁becoming ▁much ▁stronger , ▁reaching ▁wind s ▁of ▁ 1 6 0   km / h ▁( 1 0 0   m ph ). ▁Sub sequently , ▁a ▁tr ough ▁turned ▁the ▁storm ▁to ▁the ▁south west , ▁bringing ▁it ▁over ▁the ▁island ▁of ▁Ré union ▁on ▁March   1 3 . ▁In cre ased ▁wind ▁she ar ▁d eter ior ated ▁the ▁con ve ction ▁as ▁the ▁storm ▁turned ▁to ▁the ▁sout heast ▁on ▁March   1 4 . ▁The ▁next ▁day , ▁K yl ie ▁was ▁absor bed ▁by ▁the ▁tr ough . ▁ ▁On ▁Ré union , ▁K yl ie ▁produced ▁ra inf all ▁along ▁with ▁g ust s ▁of ▁over ▁ 1 0 0   km / h ▁( 6 5   km / h ), ▁along