Later, the storm made its final landfall in Móng Cái, Quảng Ninh Province in Vietnam. The storm caused moderate damage in Vietnam and killed three people. Typhoon Tokage On August 21, the JMA noted that a tropical depression had formed to the northeast of Guam. Under a favorable environment of warm sea surface temperatures, low wind shear, and very good poleward outflow, the system rapidly intensified to become Tropical Storm Tokage by early next day. Moving north-northwest, Tokage would intensify into a severe tropical storm later by the same day, and by 09:00 UTC on August 23, the JTWC upgraded Tokage to a typhoon, with the JMA following suit three hours later. The storm would peak six hours later according to the JMA, with 10-minute sustained winds of and a pressure of 970 hPa, while the JTWC estimated Tokage to have peaked at 00:00 UTC the next day, with 1-minute sustained winds of , making Tokage a Category 3-equivalent typhoon on the Saffir-Simpson scale. After peaking, Tokage rapidly weakened under high wind shear as it curved northeastwards due to a deep-layered subtropical ridge positioned to the east of the storm, and commenced extratropical transition by 03:00 UTC on August 25. The storm would complete its transition 12 hours later, with the JTWC issuing its final advisory, and the JMA following suit three hours later. Typhoon Hinnamnor (Henry) On August 27, the JTWC began monitoring a disturbance located 461 nautical miles off Iwo Jima, which they labeled Invest 90W. Following organization, the agency issued a Tropical Cyclone Formation Alert (TCFA) at 04:10 UTC the next day. 6 hours later, it intensified into a tropical storm, being named Hinnamnor by the JMA. Moving due west, Hinnamnor steadily strengthened, gaining Category 1-equivalent winds of on August 29. At the same time, the JMA upgraded Hinnamnor to a typhoon. The system underwent rapid intensification, and proceeded to gain Category 3-equivalent winds at 12:00 UTC the same day. Quickly strengthening overnight, the storm quickly grew with Category 5-equivalent winds of , with a minimum pressure of with a pinhole eye. Hinnamnor then weakened following an eyewall replacement cycle, slowing down as it neared Okinawa. As it stalled south of the Prefecture, the storm re-intensified, with an intense central dense overcast forming along with a larger eye. On August 31, at 5:30 p.m. PHT (09:30 UTC), Hinnamnor entered the PAGASA's Philippine Area of Responsibility and was