Tropical Storm Yun-yeung

On 6:00 UTC on September 4, the Joint Typhoon Warning Center (JTWC) began tracking a low-pressure area far east of Luzon.^[1] As the disturbance was in a favorable environment with low vertical wind shear and warm SSTs of 29–30 °C (84–86 °F), the JTWC issued a Tropical Cyclone Formation Alert (TCFA) on the system a day later.^[2] Soon after, the Japan Meteorological Agency (JMA) stated that the disturbance had developed into a tropical depression due to Dvorak readings.^[3] At the time, the disturbance was located in the Philippine Area of Responsibility (PAR), causing the Philippine Atmospheric, Geophysical, and Astronomical Services Administration (PAGASA) to designate the system as a tropical depression, naming it Ineng.^[4]

On 18:00 UTC on September 5, both the JTWC and JMA recognized the system as a tropical cyclone, with the latter agency naming it Yun-yeung as according to them, it had gale-force winds at the time.^[1][5] The next day, the JTWC upgraded Yun-yeung into a tropical storm.^[1] Later that day, the depression exited the PAR, causing PAGASA to cease advisories on the system.^[4] Yun-yeung steadily intensified, and early on September 7, the JMA's surface observations and Dvorak intensity estimates revealed that it had peaked with 10-minute sustained winds of 70 km/h (45 mph).^[5][6]

Due to a binary interaction with the remnants of Kirogi, Yun-yeung began to slow down, crossing into an environment with wind shear in excess of 70 km/h (45 mph). Despite that, conditions were still favorable for the system to intensify.^[7] As a result, later that day, it peaked with 1-minute sustained winds of 80 km/h (50 mph) according to the JTWC.^[1] It began tracking westward instead of north-westward, rapidly weakening due to the increasing shear.^[8] On September 8, Yun-yeung made landfall as a weak tropical depression along the northern shoreline of Suruga Bay, degenerating into a wave-like feature.^[9] Yun-yeung rapidly weakened once inland, and by September 9, had degenerated into a remnant low, causing both agencies to stop monitoring it.^[1][5]

When Yun-yeung was initially developing far from the Philippines, it with Haikui primarily enhanced the southwest monsoon, causing heavy rains in portions of Luzon.^[10] PAGASA issued a gale warning for the seaboards of portions of Northern Luzon due to the system.^[4] Yun-yeung itself caused scattered showers in Batanes, Abra, Apayao, Cagayan and Isabela.^[11]

In the Chiba and Ibaraki prefectures, heavy rain was recorded, with record high levels of rain (371.5 mm (14.63 in) in Mobara and 249.5 mm (9.82 in) in Kamogawa) seen on September 8. Some train lines were impacted in the Kanto region, since JR East suspended some lines and limited express trains.^[12] Additionally, rides in the Tokaido Line, Uchibo Line and Gaibo Line were temporarily suspended.^[13] Osaka recorded 323 mm (12.7 in) of rainfall. Due to the storm, nearly 10,000 households had temporarily lost power in Japan. Additionally, 32 local flights had to be cancelled due to Yun-yeung.^[14]

In Shinjuku Station, water leaked in an underground passage and flooded around 15 meters (49 ft) of walkway.^[15] Over 2,600 homes suffered some damage,^[16] while 77 buildings were flooded.^[17] Over 100 landslides occurred throughout Japan.^[18] Economic losses from the storm were in the tens of millions according to Aon.^[19] A total of 3 people died due to the storm.^[20] These were an elderly man who fell into a drainage ditch in Iwaki,^[21] a young man who drowned in a river,^[22] and a police officer who fell off a building.^[17]

• JTWC Best Track Data
• JMA Best Track Data
• PAGASA Tropical Cyclone Bulletins