Meteorological history | |
---|---|
Formed | September 16,1964 |
Dissipated | September 25,1964 |
Unknown-strength storm | |
10-minute sustained (JMA) | |
Lowest pressure | 895 hPa (mbar);26.43 inHg |
Category 5-equivalent super typhoon | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 280 km/h (175 mph) |
Overall effects | |
Fatalities | 43 |
Damage | Unknown |
Areas affected | Mariana Islands,Japan |
IBTrACS | |
Part of the 1964 Pacific typhoon season |
Typhoon Wilda was an intense typhoon that was tied for lowest central pressure of any typhoon in 1964,along with Typhoon Sally. [1] As the twenty-fourth named storm of the season,it origins can be traced back to when it was as a tropical storm east-southeast of Guam on September 16. Wilda moved northwestward for multiple days. it was identified as a tropical storm by Joint Typhoon Warning Center on September 19,strengthening into a typhoon that day. It reached its peak intensity over the Philippine Sea. Wilda slightly weakened following peak strength before curving northward and making landfall on September 24. The storm would eventually emerge into the Sea of Japan and curve northeast. Wilda made a final landfall on September 25 as a tropical storm,thereafter,departing Japan and quickly moving towards the central Aleutian Islands as a powerful extratropical cyclone,dissipating on September 27.
According to data from the Japan Meteorological Agency, Wilda began as a tropical storm east-southeast of Guam on September 16, marked by a large mass of clouds and associated rainbands. [2] [3] : 141 The system tracked northwest over the Northern Mariana Islands and into the Philippine Sea two days later. [2] The Joint Typhoon Warning Center recognized the storm as a tropical cyclone on September 19 when it was located roughly 370 km (230 mi) northwest of Saipan and assessed Wilda to have strengthened into a typhoon later that day. [4] : 77 An eye emerged on Nimbus satellite imagery on September 20, [3] : 159 and on September 21, Wilda reached its peak intensity over the Philippine Sea with one-minute maximum sustained winds of 280 km/h (170 mph) as estimated by the JTWC and a minimum central pressure of 895 hPa (mbar; 26.43 inHg). [2] Based on data from the JMA, this was tied for lowest central pressure of any typhoon in 1964, along with Typhoon Sally. [1] Wilda slightly weakened following peak strength before curving northward and making landfall on Kagoshima on September 24; one-minute sustained winds three hours prior to landfall were estimated to be 185 km/h (115 mph). [2] The storm passed over Shikoku and southern Honshu before emerging into the Sea of Japan and curving northeast. Wilda made a final landfall on the western coast of northern Honshu on September 25 as a tropical storm, thereafter, departing Japan and quickly moving towards the central Aleutian Islands as a powerful extratropical cyclone. [2] [4] : 77 The storm was last identified on September 27. [2]
Wilda was one of the strongest typhoons to ever strike Japan as measured by atmospheric pressure, reaching Cape Sata in Kagoshima with a central pressure of 940 hPa (mbar; 27.76 inHg). [5] The typhoon caused 47 fatalities and 530 injuries in Japan. Over 70,000 homes were destroyed and nearly 45,000 were inundated by the typhoon across the country, [6] leaving thousands of people homeless. [7] The southern and eastern coasts of Kyushu, the southern coast of Shikoku, and Hyōgo Prefecture experienced the highest proportion of destroyed homes per capita. [8] At least 64 ships were sunk with another 192 damaged or lost. [9] Damage was widespread in the northern Ryukyu Islands. [4] : 77 Banana, sugar cane, and vegetable fields in Amami Ōshima were badly damaged, along with roofs and windows. Naze lost power during the storm. Wilda brought 6-meter (20-foot) waves to southern Kyushu. [10] One British freighter ran aground off Kagoshima and broke into two; all 41 crew were rescued. [11] The widespread flooding in the region overtopped dikes and disrupted air and rail traffic. [12] At Uwajima, Ehime, a peak wind gust of 259 km/h (161 mph) was observed; [8] this was the strongest wind recorded in connection with the Wilda in Japan. [13] An 8,547-ton Indonesian freighter with 53 crew ran aground and keeled over at the Port of Kobe. [14] [15] Gale-force winds from Wilda reached the Tokyo area, damaging roofs at the Tokyo Olympic Village and uprooting trees two weeks before the start of the 1964 Summer Olympics. [16] [17] [18] A ship just south of Tokyo Bay reported winds of 76 km/h (47 mph). [4] : 77
The 1959 Pacific typhoon season was regarded as one of the most devastating years for Pacific typhoons on record, with China, Japan and South Korea sustaining catastrophic losses. It was an event in the annual cycle of tropical cyclone formation. The season had no official bounds, but tropical cyclones in the Western Pacific Ocean normally develop between May and October.
The 1964 Pacific typhoon season was the most active tropical cyclone season recorded globally, with a total of 39 tropical storms forming. It had no official bounds; it ran year-round in 1964, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1963 Pacific typhoon season has no official bounds; it ran year-round in 1963, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1951 Pacific typhoon season was a generally average season with multiple tropical cyclones striking the Philippines. With the exception of January, each month saw at least one tropical system develop; October was the most active month with four tropical cyclones forming. Overall, there were 31 tropical depressions, of which 25 became tropical storms; of those, there were 16 typhoons.
Typhoon Prapiroon, known in the Philippines as Typhoon Lusing, was the costliest tropical cyclone to strike the Korean Peninsula and the tenth costliest in the West Pacific on record, as of August 2023.
Typhoon Billie was the first typhoon officially monitored by the Joint Typhoon Warning Center. The storm brought floods to several East Asian countries in July 1959. Billie developed from a tropical disturbance west of Kiribati on July 12. Situated within favorable conditions, the system quickly reached tropical storm intensity before strengthening further to typhoon status a day after formation. Intensification continued until Billie reached its peak intensity on July 14 east of Taiwan with maximum sustained winds of 165 km/h (103 mph) and a minimum barometric pressure of 970 mbar. Slight weakening occurred before the typhoon made landfall on Zhejiang in China on July 16. After tracking inland, Billie curved northward and moved over the Yellow Sea before making a final landfall on North Korea on July 17; the storm transitioned into an extratropical cyclone shortly afterwards before dissipating over the Sea of Japan a day later.
Typhoon Caitlin, known in the Philippines as Typhoon Ising, contributed to major drought relief in Okinawa. A tropical disturbance formed in the middle of July 1991 in the eastern portion of the Western Pacific monsoon trough, and while tracking to the west-northwest, was designated a tropical depression on July 21. Thunderstorm activity associated with the depression increased markedly on July 22, and two days later, the depression was upgraded into Tropical Storm Caitlin. The storm turned northward as it rounded a subtropical ridge while gradually intensifying. Caitlin became a typhoon on July 25 and peaked in intensity on July 27 near Okinawa. The typhoon began to weaken as it turned northeast over the Korea Strait. On July 30, Catlin transitioned into an extratropical cyclone as it entered the Sea of Japan.
Typhoon Chaba was the strongest tropical cyclone in the western Pacific during 2004 and caused a swath of damage from the Mariana Islands to Japan from August through September of that year. Chaba was the Japan's second costliest storm during the season, only behind Songda in September, and peaked as a typhoon with maximum sustained winds equivalent to that of a Category 5 on the Saffir–Simpson hurricane wind scale.
Typhoon Flo, known in the Philippines as Typhoon Norming, was a long-lived typhoon that brought destruction to much of Japan during September 1990. Flo originated from an area of convection that first formed to the southeast of the Marshall Islands on September 7. Five days later, the disturbance obtained tropical depression status, and on September 13, intensified into a tropical storm. Tracking west-northwest as it rounded a subtropical ridge, Flo slowly deepened, and on September 15, became a typhoon. After developing an eye, Flo began to rapidly intensify, and on September 17, Flo attained peak intensity. Shortly thereafter, the typhoon began to recurve to the northeast towards Honshu in response to deepening troughs to the northwest and north of the system, which resulted in a weakening trend due to increased vertical wind shear despite remaining over warm water. On September 19, Flo made landfall on southern Honshu, becoming the first typhoon to hit the Kii Peninsula in 11 years, and thereafter started to transition into an extratropical cyclone. The extratropical remnants of Flo were last noted on the morning of September 22.
Typhoon Yancy, known in the Philippines as Typhoon Tasing, was one of the costliest and most intense tropical cyclones to strike Japan on record. Yancy was the sixth typhoon of the annual typhoon season and sixth tropical cyclone overall to impact Japan that year. Developing out of an area of disturbed weather in the open northwest Pacific on August 29, 1993, the precursor to Yancy tracked westward and quickly intensified to reach tropical storm strength on August 30. Just two days later, the tropical storm reached typhoon intensity as it recurved towards the northeast. A period of rapid intensification followed, allowing Yancy to quickly reach super typhoon intensity. The strong tropical cyclone reached peak intensity on September 2 with maximum sustained winds of 175 km/h (109 mph). The following day Yancy made its first landfall on Iōjima at nearly the same strength; over the course of the day the typhoon would make three subsequent landfalls on Japanese islands. Land interaction forced the tropical cyclone to weaken, and after its final landfall on Hiroshima Prefecture, Yancy weakened below typhoon intensity. After emerging into the Sea of Japan, Yancy transitioned into an extratropical cyclone; these remnants persisted as they meandered in the sea before dissipating completely on September 7.
Typhoon Khanun, known in the Philippines as Typhoon Kiko, was the strongest tropical cyclone to make landfall on Zhejiang Province since Wanda in 1956. Khanun developed from an area of convection east-southeast of Yap on September 5, thereafter tracking northwestward. The precursor reached tropical storm status on September 7 and typhoon intensity the next day. The tropical cyclone reached its peak intensity on September 10 with winds estimated at 155 km/h (100 mph) and a minimum barometric pressure of 945 mbar. After weakening slightly, Khanun moved ashore Zhejiang Province the next day, weakening further as it tracked over land. After recurving into the Yellow Sea on September 12, Khanun became extratropical; these remnants continued to track into the open North Pacific before they were last noted on September 16.
Typhoon Zola struck Japan during August 1990. An area of disturbed weather developed during mid-August to the west of Guam. The disturbance developed into a tropical depression on August 16 while tracking eastward. Decreased wind shear aided in intensification, and it is estimated that the depression strengthened into a tropical storm on August 17. Continuing to intensify, Zola turned northwest in response to a subtropical ridge to its east before obtaining typhoon intensity on August 20. Typhoon Zola reached its peak intensity the next day. After weakening slightly, the storm moved ashore on Honshu. On August 23, the system transitioned into an extratropical cyclone over the Sea of Japan.
Typhoon Hattie, known in the Philippines as Typhoon Pasing, was the fifth tropical cyclone of a record-six to hit Japan during the 1990 Pacific typhoon season. Hattie originated from an area of disturbed weather that developed within the Western Pacific monsoon trough towards the end of September. Tracking westward, the disturbance initially was slow to develop, although on September 30, the system was classified as a tropical depression. Following an improvement of its convective structure and an increase in associated convection, the depression was upgraded into Tropical Storm Hattie on October 1. Following the development of an eye, Hattie attained typhoon intensity on October 2. The typhoon continued to slowly deepen as its forward speed slowed. Despite a decrease in cloud top temperatures around the eye, Hattie was estimated to have attained peak intensity on October 5. After recurving to the north and then northeast, Hattie began to slowly weaken due to increased wind shear. On October 7, Hattie lost typhoon intensity, and after tracking directly over Tokyo, transitioned into an extratropical cyclone on the next day.
Typhoon Kinna, known in the Philippines as Typhoon Neneng, was a mid-season typhoon that struck Japan during 1991. An area of disturbed weather formed within the Western Pacific monsoon trough during early September 1991. The disturbance was upgraded into a tropical depression on September 10 after an increase in organization. Tracking northwest due to a weak subtropical ridge to its north, the depression strengthened into a tropical storm at 00:00 UTC on September 11. Later that day, Kinna was upgraded into a severe tropical storm. Following the development of a poorly defined eye, Kinna was upgraded into a typhoon on September 12. The cyclone turned north in response to a trough and passed through Okinawa as a minimal typhoon. Typhoon Kinna obtained peak intensity on September 13, but thereafter, Kinna accelerated north-northeastward toward Kyushu, passing over the island that day at peak intensity. Typhoon Kinna rapidly transitioned into an extratropical low as it tracked along the northern coast of Honshu. Its extratropical remnants were last noted on the evening of September 16.
Typhoon Janis, known in the Philippines as Typhoon Gloring, was an early-season typhoon that struck Japan during August 1992. An area of disturbed weather formed near Pohnpei in late-July 1992, and after an increase in thunderstorm activity, a tropical depression developed on August 3. After passing near Guam, Janis tracked generally westward, and on August 5, the storm was believed to have attained typhoon intensity. After intensifying at a brisk pace, Janis attained peak intensity on August 6 near Okinawa. Thereafter, the typhoon began to weaken and accelerate as it recurved towards Kyushu, where it made landfall on the next day. Land interaction took its toll on the typhoon as it tracked northeast, paralleling the western coast of Honshu. On August 9, Janis transitioned into an extratropical low over Hokkaido.
Tropical Storm Percy, known in the Philippines as Tropical Storm Miling, was an early-season tropical cyclone that passed through Japan during July 1993. An area of disturbed weather developed in the Philippine Sea on July 26. Gradual development ensued and on July 27, the disturbance was classified as a tropical depression. The following morning, the depression was upgraded into Tropical Storm Percy. Moving north-northwest, Percy slowly deepened and obtained its peak intensity of 115 km/h (70 mph) and a minimum barometric pressure of 975 mbar (28.79 inHg). Late on July 29, Percy passed over Kyushu and began to weaken. Percy was downgraded to a tropical depression on July 30 and dissipated completely two days later.
Typhoon Robyn, known in the Philippines as Typhoon Openg, was a mid-season tropical cyclone that brushed Japan during August 1993. Typhoon Robyn originated from a near equatorial monsoon trough in the eastern Caroline Islands in late July. Tracking west-northwest, a tropical depression developed on August 1, and became a tropical storm the next day. Following an increase in organization, Robyn obtained typhoon intensity on August 5. The typhoon briefly tracked west before veering to the northwest while intensifying. On August 7, Robyn attained its peak intensity of 160 km/h (99 mph), with a barometric pressure of 940 mbar (28 inHg). After passing through the Ryukyu Islands, Robyn skirted past western Kyushu on August 9 while steadily weakening. Midday on August 10, Robyn lost typhoon intensity over the Sea of Japan. The next day, the system was declared an extratropical cyclone.
Typhoon Louise and Tropical Storm Marge, known in the Philippines as Typhoon Ining and Tropical Storm Liling, respectively, were a pair of tropical cyclones that impacted Palau and the Philippines in November 1964. Louise was one of the most destructive typhoons documented in the central Philippines. Tracking data from meteorological agencies disagree whether the systems were a single tropical cyclone or two distinct tropical cyclones that occurred in quick succession, named separately by the Joint Typhoon Warning Center (JTWC) as Louise and Marge.
Typhoon Kathy, known in the Philippines as Typhoon Welpring, was the largest and longest-lived typhoon in 1964. As the fourteenth named storm of the season, it originated from an area of circulation southeast of Japan by August 11. The following day, the system strengthened into a tropical storm, gaining the name Kathy. Kathy reached typhoon strength on August 13, passing south of Tokyo, approaching the Ryukyu Islands. The typhoon's winds peaked at 165 km/h (103 mph) on August 14, before tapering as the storm curved west-southwest. For the next four days, Kathy and nearby Typhoon Marie began a Fujiwhara interaction, causing both storms to rotate around each other, which ended when Marie was pulled into Kathy's circulation. Between August 15 and August 16, Kathy weakened into a tropical storm, before strengthening back to typhoon status. The storm's west-southwest path brought the center across the Ryukyu Islands and near Okinawa on August 16 as Kathy began to execute a loop in its track. Two days later, Kathy's winds were estimated by the JTWC to be around 215 km/h (134 mph). The typhoon's track made a smaller loop on August 20, before heading northwards. On August 23, Kathy made landfall in Japan with winds of 130 km/h (81 mph) and weakened to a tropical storm. It then curved northeast. On August 25, Kathy transitioned into an extratropical cyclone and continued northeast, reaching the Bering Strait on September 1. Due to its lifetime and large size, the Joint Typhoon Warning Center issued warnings for 13+1⁄2 days, and the storm's circulation reached a radius of 1,370 kilometres (850 mi).
Typhoon Opal, known in the Philippines as Super Typhoon Naning, was an intense Category 5-equivalent typhoon in the extremely active 1964 Pacific typhoon season. Opal also had the largest wind circulation of any typhoon in 1964, with a total span of 2,100 km (1,300 mi).Data from the Joint Typhoon Warning Center (JTWC) indicated that Opal's winds were the highest of any typhoon in 1964. As the thirty-ninth named storm and the twenty-sixth typhoon of the season, it originated from a tropical wave in early December, with its wind circulation developing by December 8. This system quickly organized, gaining the name Opal, and reaching typhoon status on December 9. Opal moved through Yap and Palau for two days. On that last day, Opal reached its peak intensity with one-minute sustained winds of 315 km/h (196 mph) and a central pressure of 895 hPa (26.43 inHg). On December 14, Opal passed north of some Filipino islands and its winds began to lose intensity. Later that day, Opal made landfall in the Philippines with one-minute sustained winds of 140 km/h (87 mph). Opal weakened further as it moved over Luzon. Its center then executed a small counterclockwise loop over western Luzon before curving north and briefly emerging into Lingayen Gulf as a tropical storm. Opal crossed northwestern Luzon and the Babuyan Islands on December 16 and later became extratropical near Okinawa on December 17; this phase of Opal's development dissipated the next day.