 Tropical Storm Linfa developed as a tropical depression just off the western coast of Luzon on May 25 . The disturbance quickly intensified to reach tropical storm intensity a few hours after cyclogenesis . However , intensification leveled off as Linfa executed a small clockwise loop before a subsequent landfall on Luzon on May 27 . Due to land interaction the storm temporarily weakened and decoupled before reforming in the Philippine Sea . Afterwards Linfa began reintensifying and reached its peak intensity on May 29 with maximum sustained winds of 100 km / h ( 65 mph ) and a barometric pressure of 980 mbar ( hPa ; 28 @.@ 94 inHg ) . Following its peak the tropical storm began to deteriorate and transitioned into an extratropical cyclone on May 30 ; these extratropical remnants continued to track northward through Japan before dissipating in the Sea of Okhotsk on June 4 . 
 Tropical Storm Linfa developed as a tropical depression just off the western coast of Luzon on May 25 . The disturbance quickly intensified to reach tropical storm intensity a few hours after cyclogenesis . However , intensification leveled off as Linfa executed a small clockwise loop before a subsequent landfall on Luzon on May 27 . Due to land interaction the storm temporarily weakened and decoupled before reforming in the Philippine Sea . Afterwards Linfa began reintensifying and reached its peak intensity on May 29 with maximum sustained winds of 100 km / h ( 65 mph ) and a barometric pressure of 980 mbar ( hPa ; 28 @.@ 94 inHg ) . Following its peak the tropical storm began to deteriorate and transitioned into an extratropical cyclone on May 30 ; these extratropical remnants continued to track northward through Japan before dissipating in the Sea of Okhotsk on June 4 . 
Tropical Storm Linfa developed as a tropical depression just off the western coast of Luzon on May 25 . The disturbance quickly intensified to reach tropical storm intensity a few hours after cyclogenesis . However , intensification leveled offf as Linfa executed a small clockwise loop before a subsequent landfall on Luzon on May 27 . Due to land interaction da storm temporarily weakened and decoupled b4 reforming in the Philippine Sea . Afterwards Linfa began reintensifying and reached its peak intensity on May 29 with maximum sustained winds of 100 km / h ( 65 mph ) and a barometric pressure of 980 mbar ( hPa ; 28 @.@ 94 inHg ) . Following its peak the tropical storm began to deteriorate and transitioned into an extratropical cyclone on May 30 ; these extratropical remnants continued to track northward through Japan befob4sipating in the Sea of Okhotsk on June 4 .