An area of convection active for the previous 48 hours led to the formation of a low level circulation near 23°N 151°E early on July 27. Gradual intensification ensued, and the system developed into a tropical depression that evening, a tropical storm on July 28, and a typhoon by July 31 as it moved west-northwest. The cyclone struck southern Kyūshū, in Japan, early on July 31 which weakened the cyclone. The tropical storm then moved into the East China Sea which continuing to spin down. Upper level wind shear took its toll, leading to its weakening into a tropical depression and its ultimate dissipation in the Yellow Sea along the west coast of Korea.
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