Typhoon Holly (1984)

Map plotting the track and the intensity of the storm, according to the Saffir–Simpson scale

While Tropical Storm Gerald was forming in the South China Sea, the Western Pacific monsoon trough extended eastward in the middle of August 1984. By noon on August 13, the monsoon trough extended from Tropical Depression 9W to just northwest of Guam, and within 36 hours, this trough moved northwest and became sharper, with surface barometric pressures of 1000 mbar (30 inHg) and winds of 40 to 50 km/h (25 to 30 mph). Organization of the convection gradually improved and satellite imagery indicated that a surface low was forming. The Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert (TCFA) at 15:15 UTC on August 14. At 00:00 UTC on the next day, a Hurricane Hunter aircraft investigated the system, measuring a pressure of 998 mbar (29.5 inHg).[2] This prompted the Japan Meteorological Agency (JMA) to upgrade the low into a tropical depression.[3][nb 1]

At noon on August 15, synoptic data suggested that the system did not have a closed circulation; however, ship reports suggested that it was producing gale-force winds at the time. Early on August 16, a second aircraft investigated the system, finding a pressure of 992 mbar (29.3 inHg) and a closed circulation.[2] This promoted the JTWC to classify the system as Tropical Storm Holly while the JMA upgraded Holly directly to severe tropical storm.[5][nb 2] Despite its large size, Holly slowly deepened,[2] and was upgraded to a typhoon by the JMA at noon on August 17.[3] Nevertheless, Holly remained fairly disorganized, with aircraft observing light winds near the center and the strongest winds located in a rainband 110 to 280 km (70 to 175 mi) northeast from the center. It was not until August 18 that aircraft observed surface wind gusts of over 95 km/h (60 mph).[2] At 00:00 UTC that day, the JTWC upgraded Holly into a typhoon while the storm was located near Okinawa.[7]

After initially tracking westward under the influence of a subtropical ridge, Holly turned northwest for about a 30 hour period before turning north as it rounded the western side of the ridge.[2] At noon on August 19, the JTWC reported that Holly attained its peak intensity of 135 km/h (85 mph) while the JMA reported that Holly reached its highest winds of 130 km/h (80 mph) and a minimum pressure of 960 mbar (28 inHg). Shortly after its peak, Holly turned northeast while also accelerating in response to the westerlies, which sent the storm across the Korean Straits on a collision course with the Korean Peninsula. Land interaction with South Korea resulted in a weakening trend, with both the JTWC and JMA downgrading Holly to a tropical storm. Upon entering the Sea of Japan, Holly began to transition into an extratropical cyclone. The low-level circulation quickly became exposed from the center, and what little convection remained was far removed from the center, and attached to a cold front.[2] At 06:00 UTC on August 21, Holly was declared extratropical by the JMA,[3] with the JTWC following suit 12 hours later.[2] Two days later, the JMA had ceased tracking the cyclone altogether.[3]

Typhoon warnings were posted for Cheju Island and up to 80 km (50 mi) inland across South Korea. Ferry service between Cheju and the mainland was canceled due to the impeding threat of rough seas,[8] prompting 800 fishing boats to seek shelter.[8] Throughout South Korea, nine people were killed or missing and hundreds lost their homes. At least 10 fishing boats were demolished, hundreds of hectares of farmland were flooded, and several homes were damaged.[7]

In some places of the southern portion of the island of Kyushu, forecasters anticipated that up to 280 mm (11 in) of rain could fall.[9] Across the Ryukyu Islands, 15,000 air travelers were stranded.[10] In Naha, the main city in Okinawa, an estimated 14,000 tourists were stranded when all 23 scheduled flights to Japanese main islands were canceled.[9] Between the Ryukyu Islands and the Japanese mainland, ferry service was called off for two days, resulting in 21,000 stranded passengers.[8] Further north, in Itsuki, 31 people lost their homes. Forty-one flights were cancelled in Miyazaki Prefecture, which caused an additional 4,200 stranded travelers.[11] Overall, the storm dropped heavy rainfall across much of Japan.[12] A peak rainfall total of 708 mm (27.9 in) occurred at Ebino, including 338 mm (13.3 in) in a day.[13] Within 24 hours, 433 mm (17.0 in) of rain fell in Mount Yonaha, including 48 mm (1.9 in) an hour.[14] Moreover, a wind gust of 108 km/h (67 mph) was recorded in Mount Yonaha[15] while further south, wind gusts of 95 mph (153 km/h) were recorded in Okinawa.[9] Nation-wide, one person was killed due to high waves in Nagasaki,[16] nine were listed as missing,[2] and eleven were wounded, including nine in Okinawa and the western prefectures of Kumamoto, Nagaski, Yamaguchi, and Hiroshima while two in Aichi Province sustained injuries after strong winds toppled a tree. Property damage was estimated at US$1 million.[16]

The extratropical remnants caused significant flooding in the Russian Far East. Water levels around Khabarovsk along the Amur River rose 10 m (33 ft) to 51 m (167 ft), marking one of the few times the river reached that high since records began in the area in 1895.[17][18] Due to the subsequent flooding, 64 families were evacuated, although 2,000 cows and pigs were left stranded. Further west, in Arkhara, a dam along the Amur River bursts its banks along a 20.1 km (12.5 mi) stretch, resulting in the river's worst flooding since 1928 and the evacuation of many stranded children in helicopters.[17]

• Typhoon Pat (1985)