landfall south of Shanghai. Although the JTWC issued its final advisory at 00:00 UTC on August 8, with the JMA doing the same 36 hours later, its remains could still be identified through August 10. Tropical Storm Bill, which formed on August 5 east of Taiwan, moved northwest to hit eastern China as a 45 mph tropical storm. Torrential rains and heavy flooding resulted in 110 casualties and widespread damage to roads and dams. Tropical Storm Clara An area of disorganized convection about north of Wake Island in early August. The disturbance was classified on August 5 by the JMA. The depression tracked westward under the influence of a subtropical ridge. Two days later, the system began to organize, although shower activity remained exposed from the center. Strong wind shear prevented further development, but by August 10, thunderstorm activity had increased in coverage. At 19:15 UTC the same day, the JTWC upgraded it to Tropical Storm Clara, with the JMA following suit around the same time. Due to a strengthening ridge, Kevin performed a counterclockwise loop, only to turn northeast on August 11. Around this time, the JTWC and JMA estimated that Clara attained peak winds of . Shortly afterwards, shower activity quickly became displaced from the deep convection, prompting a weakening trend. The JTWC issued its final warning on August 12, though the JMA did not following suit until four days later. JMA Tropical Storm Eleven This was not tracked by the JTWC. Typhoon Doyle On August 12, an westward-moving area of disturbed weather developed within the monsoon trough. Deep convection developed near the low-level center on the next day, and the JMA classified the disturbance as a tropical depression. Overnight August 13 into August 14, the depression began to organize, and after performing a counterclockwise loop, it began moving to the west-northwest. At 18:00 UTC the same day, the JMA upgraded the depression into a tropical storm, though the JTWC did not follow suit until 18 hours later. Doyle then entered a period of rapid deepening, with the JMA upgrading Doyle into a typhoon on the morning of August 16. At 18:00 UTC, the JTWC estimated that Doyle attained peak winds of , although according to the JMA, Doyle did not reach its peak intensity of . The typhoon then curved north as it rounded a subtropical ridge, although unlike most recurving tropical cyclones, a TUTT cell prevented.