A tropical disturbance formed southeast of Guam on July 19 and tracked westward steadily. After issuing a Tropical Cyclone Formation Alert on July 21, the Joint Typhoon Warning Center upgraded the system to a tropical depression early on July 22, although the location of its low-level circulation center was not clear. The Japan Meteorological Agency, however, kept reporting it as a low-pressure area until it was upgraded to a tropical depression late on July 23. After the slow consolidation for several days, the system was upgraded to a tropical storm near Okinotorishima at around 18:00 on July 24 by agencies such as JMA and JTWC, with an international name Jongdari. A microwave imagery revealed a low-level forming eyewall next day, indicating a consolidating system. After JMA upgraded Jongdari to a severe tropical storm at noon, the system accelerated northeastward under the influence of a near-equatorial ridge to the south. On July 26, as Jongdari started to interact with an upper-level cold-core low to the north which significantly enhanced poleward outflow, it intensified to a typhoon in the afternoon despite increasingly unfavorable vertical wind shear. Over the warm sea surface temperatures between near the Ogasawara Islands, JMA reported that Jongdari had reached peak intensity at 00:00 UTC on July 27, with ten-minute maximum sustained winds of 140 km/h, and a minimum central pressure of 965 hPa. Although JTWC indicated Jongdari reached peak intensity at 12:00 UTC with one-minute maximum sustained winds of 175 km/h, the rugged eye of Jongdari kept periodically visible with an elongated structure due to the further interaction of the upper-level low which had moved to the northwest side of the typhoon. As the steering influence transitioned to a subtropical ridge to the northeast, Jongdari executed a rare counter-clockwise turn to the southeast of Japan. Jongdari began to be inundated by subsidence on July 28, as the Fujiwhara effect had made the upper-level low move to the west of the typhoon. It also initiated a weakening trend while accelerating northwestward and then westward toward the Japanese island of Honshu. At around 01:00 JST on July 29, Typhoon Jongdari made landfall over Ise, Mie Prefecture with ten-minute maximum sustained winds at 120 km/h and the central pressure at 975 hPa. The storm weakened rapidly inland and made its second landfall over Buzen, Fukuoka Prefecture, at around 17:30 JST, with ten-minute sustained winds of 75 km/h and a central pressure of 992 hPa. At around 10:30 CST on August 3, Tropical Storm Jongdari made landfall over Jinshan District, Shanghai. Jongdari rapidly weakened after landfall, dissipating on the next day.
Impact
Japan
24 people were injured when the typhoon hit Japan. JR-West train services were delayed or cancelled due to the storm. Although Jongdari didn't directly hit Hokuriku region, it did bring föhn wind to the area because it is located at the leeward slope of the Japanese Alps. Niigata prefecture recorded temperatures close to. Agricultural damage in Chiba and Aichi Prefecture were about JP¥1.59 billion. Preliminary industry loss were estimated between US$1.4–2 billion.
China
Total damage from Jongdari were about CN¥420 million.
