Meteorological history | |
---|---|
Formed | October 14,1970 |
Dissipated | October 25,1970 |
Typhoon | |
10-minute sustained (JMA) | |
Lowest pressure | 940 hPa (mbar);27.76 inHg |
Category 4-equivalent super typhoon | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 240 km/h (150 mph) |
Lowest pressure | 941 hPa (mbar);27.79 inHg |
Overall effects | |
Fatalities | 631 |
Missing | 284 |
Damage | $50 million (1970 USD) |
Areas affected | Philippines,Indonesia,Vietnam |
IBTrACS | |
Part of the 1970 Pacific typhoon season |
Typhoon Kate,known in the Philippines as Typhoon Titang, [1] was the second of two super typhoons to strike the Philippines within a week in October 1970,the first being Super Typhoon Joan. As a result,Kate produced heavy damage and over 631 casualties. At the time,Kate was one of the deadliest typhoons to strike the Philippines.
Super Typhoon Kate was first identified by the Joint Typhoon Warning Center (JTWC) on October 7, 1970, and by the Japan Meteorological Agency on October 9, 1970 as a tropical disturbance near the Marshall Islands. The system tracked in a general westward direction and relocated itself further south during this period in response to Typhoon Joan wake to the northwest. By October 13, convection sharply increased as the system entered a region of strong diffluence. The following day, the disturbance featured a marked increase in organization as thunderstorms continued to consolidate around the center of circulation. During the afternoon of October 15, reconnaissance aircraft reached the storm and reported that it was already nearing typhoon status. Sustained winds were measured at 110 km/h (68 mph) along with a barometric pressure of 985 mbar (hPa; 29.12 inHg). [2] At this time the storm was classified as Tropical Storm Kate, the 18th named storm of the 1970 season. [3] Additionally, the storm had begun developing an eyewall, an indication that the system was likely to intensify further. Over the following three days, the storm continued its westward track while gaining strength. [2]
Throughout the day on October 16, Kate underwent a period of rapid intensification. During this time, sustained winds increased from 140 to 215 km/h (87 to 134 mph), ranking Kate as a Category 4 typhoon on the modern day Saffir–Simpson Hurricane Scale. [4] Early on October 17, reconnaissance planes flown into the typhoon measured the eye to be 18.5 km (11.5 mi) in diameter. Although winds were still increasing, the lowest pressure recorded in relation to Kate was measured at this time at 940 mbar (hPa; 27.7 inHg). [5] Further intensification ensued as the typhoon neared the southeastern Philippine island of Mindanao on October 18. Just before making a rare landfall roughly 45 km (28 mi) south of Davao City in the Davao Region, Kate attained its peak winds of 240 km/h (150 mph), classifying it as a super typhoon according to the JTWC. [4] As the storm moved over land, the eye abruptly shrank to 7.4 km (4.6 mi) in diameter but this feature dissipated hours later. [5]
Due to the interaction with the mountainous terrain of Mindanao, Kate quickly weakened as it moved northwestward across the archipelago. By October 19, the system had weakened to a tropical storm, less than 24 hours after attaining its peak winds. [4] Despite the notable weakening, the structure of the storm remained relatively intact as it moved over the Sulu Sea. [2] Throughout the day, the system briefly sped up before rapidly slowing near the South China Sea. [4] On October 20, decreased interaction with land allowed Kate to re-attain typhoon status just before passing over Busuanga Island. [2] Continuing its northwest track, the typhoon slowly intensified and redeveloped a 37 mi (23 mi) wide eye. Late on October 21, the JTWC assessed the storm to have re-attained Category 4 intensity; [5] however, post-storm analysis indicated that sustained winds did not exceed 195 km/h (121 mph). [4] The following day, a ridge to the north of Kate prevented the system from tracking further north and prompted a west-southwestward track. [6]
Gradual weakening took place over the following several days as Kate slowly neared the Indochina coastline. By October 24, winds had decreased below 155 km/h (96 mph) and the eye became asymmetrical and partially open in the northeast quadrant. [4] [7] On October 25, the typhoon further weakened to a tropical storm just off the coast of Vietnam. Later that day, the system made its final landfall near Da Nang, Vietnam with winds of 100 km/h (62 mph). [4] [6] Rapid weakening ensued as Kate moved over the high terrain of southeast Asia, with the storm degrading to a tropical depression within six hours of moving inland. [4] The system dissipated within the next 24 hours as it moved over the plateau region of Cambodia. [6] Both JTWC and JMA released their final advisories as Kate dissipated over Vietnam.
Mindanao is situated outside the typhoon belt due to its close proximity to the equator. Typhoons rarely hit the island, often curving northward and making landfall in the more northern parts of the country. When Kate made landfall in southern Mindanao, the large loss of life from the typhoon is thought to be related to the lack of tropical cyclone experience for its residents. [2]
In southern Mindanao, over 5,000 houses and other such structures were damaged or destroyed by storm surge, heavy rains and strong winds produced by Typhoon Kate. Damage from the storm was estimated at $50 million, making it one of the costliest typhoons on record at the time. A total of 631 people were confirmed to have been killed by the storm and 284 others were listed as missing, ranking Kate as one of the deadliest typhoons to strike the Philippines at the time. [2] An American newspaper, The Lewiston Daily Sun (now known as the Sun Journal ) erroneously dubbed Kate as the deadliest typhoon to ever hit the Philippines, as the 1881 Haiphong typhoon and typhoons Amy and Trix in the early 1950s had higher death tolls compared to Kate (higher than 900 fatalities). [8] The paper also erroneously stated that the previous deadliest typhoon in the Philippines was a storm in the 1960s which killed 200 people in Manila – possibly referring to either Tropical Storm Lucille in 1960, Typhoon Patsy in 1962 or Typhoon Winnie in 1964. [8]
Initial reports from the Red Cross indicated that at least 150 homes were destroyed within hours of Kate's landfall. Telecommunication was lost to much of the region as power lines were down after being pummeled by high winds. [9] Within a day of the storm's passage, the death toll had reached 13 with 29 others missing and was expected to increase. [10]
Due to the threat of the typhoon, United States military officials prompted the evacuation of a military hospital near Da Nang and the relocation of aircraft. The level of fighting during Kate's passage was regarded as one of the lowest during the Vietnam War as most tactical bombing missions were canceled. During the 24 hours in which the storm affected Vietnam, the United States launched 46 air bombings, the fewest in over two years. [11] Although damage estimates and reports of deaths are scarce out of Vietnam, floodwaters, considered the worst since 1964, affected an area nearly 140 square miles (360 km2) south of Da Nang. Roughly 900 people were evacuated the first day after Kate by Marine Aircraft Group 16, and over 9,000 South Vietnamese were rescued by the 1st Marine Aircraft Wing, in Vietnam to fight the Vietnam War. [12]
The 2006 Pacific typhoon season was a destructive and deadly season, although it was near-average in terms of activity with a total of 23 named storms, 15 typhoons, and six super typhoons. Compared to the previous season, more typhoons inflicted damage across several countries, particularly China and the Philippines, some of which made landfall at higher intensities. The ratio of intense typhoons to all typhoons is at 0.73, the highest since 1970.
The 2004 Pacific typhoon season was an extremely active season that featured the second-highest ACE ever recorded in a single season, second only to 1997, which featured 29 named storms, nineteen typhoons, and six super typhoons. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2004, though most tropical cyclones typically develop between May and October. The season's first named storm and also the first typhoon, Sudal, developed on April 4, later was reached typhoon status two days later, and became the first super typhoon of the year three days later. The season's last named storm, Noru, dissipated on December 22.
The 1997 Pacific typhoon season was a record-breaking season featuring eleven tropical cyclones reaching super typhoon intensity, tying the record with 1965 with the most intense tropical cyclones globally, and was the ninth and last consecutive year of above-average tropical cyclone activity that started in 1989. Its extremely high activity produced highest ACE index ever index recorded in a single tropical cyclone season. In addition, this season had ten Saffir-Simpson Category 5-equivalent tropical cyclones, the most ever recorded, even greater than the 2005 Atlantic hurricane season, and 2020 Atlantic hurricane season, for Category 4, which had nearly half of the amount. The 1997–98 El Niño event was a contributing factor to this unusually high activity. Despite this, the season produced an average number of tropical storms, spawning 28 tropical storms.
The 1995 Pacific typhoon season was a slightly below average season in terms of named storms, ending a 6-year stretch of above average activity. It occurred all year round, though most tropical cyclones formed between May and November.
The 1992 Pacific typhoon season was the fourth consecutive above-average season, producing 31 tropical storms, 16 typhoons and five super typhoons. It had no official bounds; it ran year-round in 1992. Despite this, most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1980 Pacific typhoon season was a slightly-below average season when compared to the long-term average, though it featured several intense storms. It ran year-round in 1980, but most tropical cyclones formed between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. A total of 28 tropical depressions formed this year in the Western Pacific, of which 24 became tropical storms and were assigned a name by the Joint Typhoon Warning Center. Beginning in March, tropical cyclones formed in each subsequent month through December. Of the 24 named storms, 15 storms reached typhoon intensity, of which 2 reached super typhoon strength.
The 1970 Pacific typhoon season has no official bounds; it ran year-round in 1970, 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.
Typhoon Mike, known in the Philippines as Super Typhoon Ruping, of 1990 was the strongest typhoon to hit the Philippines since Typhoon Irma in 1981 and Typhoon Nina in 1987. Forming from an area of persistent convection over the Caroline Islands, Mike was first designated on November 6, 1990 and moved generally westward. Later that day, the depression strengthened to Tropical Storm Mike near Yap. Mike became a typhoon early on November 9, and subsequently entered a period of rapid deepening. Late on November 10, the typhoon reached its maximum intensity of 115 mph (185 km/h), as estimated by the Japanese Meteorological Agency. After weakening slightly, Mike made landfall in the central Philippines. The storm weakened considerably due to land interaction, only to briefly re-intensify on November 14. Typhoon Mike turned west-northwest and later north-northwest, avoiding land interaction with Vietnam. Vertical wind shear increased, and on November 15, Mike weakened below typhoon intensity. Early the next day, the storm passed over western Hainan Island, and degraded to a tropical depression that night. After briefly emerging into the Gulf of Tonkin, Mike passed over Northern Vietnam and southern China, where it dissipated on November 18.
This timeline documents all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation during the 2008 Pacific typhoon season. The 2008 Pacific typhoon season officially started on January 1, 2008 and ended on January 1, 2009.
The 2009 Pacific typhoon season was a below average season that spawned only 22 named storms, 13 typhoons, and five super typhoons. Despite this, it was a very deadly season, with the Philippines having experienced its deadliest season in decades due to the impact of typhoons Ketsana and Parma, while typhoon Morakot went on to become the deadliest storm to impact Taiwan in its modern history. The first half of the season was very quiet, whereas the second half of the season was extremely active. The season's first named storm, Kujira, developed on May 3, while the season's last named storm, Nida, dissipated on December 3.
The 2013 Pacific typhoon season was a devastating and catastrophic season that was the most active since 2004, and the deadliest since 1975. It featured Typhoon Haiyan, one of the most powerful storms in history, as well as one of the strongest to make landfall on record. It featured 31 named storms, 13 typhoons, and five super typhoons. The season's first named storm, Sonamu, developed on January 4 while the season's last named storm, Podul, dissipated on November 15. Collectively, the storms caused 6,829 fatalities, while total damage amounted to at least $26.41 billion (USD), making it, at the time, the costliest Pacific typhoon season on record, until it was surpassed five years later. As of 2024, it is currently ranked as the fifth-costliest typhoon season.
Typhoon Nancy, known in the Philippines as Typhoon Weling, was a destructive typhoon that moved through Vietnam and the Philippines during October 1982. The typhoon originated from an area of convection and was first classified as a tropical cyclone on October 10. The system attained gale-force winds the next day, and slowly deepened thereafter. Although Nancy initially moved west, the system maintained a general westward course for much of its duration, striking Luzon on October 14 at peak intensity of 215 km/h (130 mph). It weakened to tropical storm strength overland, but re-intensified to typhoon intensity over the South China Sea. Nancy hit northern Vietnam on the October 18, and weakened almost immediately thereafter, before dissipating on October 20 inland over Vietnam.
Severe Tropical Storm Kelly, known in the Philippines as Tropical Storm Daling, was a weak but destructive tropical storm that struck the Philippines in June 1981. A tropical disturbance organized into a tropical depression east of the Philippines on June 28. It tracked westward, reaching tropical storm on June 30 before hitting the central Philippines. Kelly weakened over the islands, but re-strengthened over the South China Sea, nearly attaining typhoon status on July 2. The system passed through the southern Hainan Island on July 3. The cyclone then crossed the Gulf of Tonkin as a weakening tropical storm, and made landfall in northern Vietnam on July 4 as a tropical storm. Kelly dissipated two days later inland.
Typhoon Hagupit known in the Philippines as Super Typhoon Ruby, was the second most intense tropical cyclone in 2014. Hagupit particularly impacted the Philippines in early December while gradually weakening, killing 18 people and causing $114 million of damage in the country. Prior to making landfall, Hagupit was considered the worst threat to the Philippines in 2014, but it was significantly smaller than 2013's Typhoon Haiyan.
Severe Tropical Storm Aere, known in the Philippines as Tropical Storm Julian, was a long-lived tropical cyclone that struck Central Vietnam in October 2016. The nineteenth named storm of the annual typhoon season, Aere formed on October 4, 2016 as a tropical depression to the east of Luzon, Philippines shortly after the JMA had started tracking Songda. On the next day, the system had become a tropical storm and it moved into South China Sea. During October 7, it intensified into a severe tropical storm and reached peak intensity with 10-minute winds of 110 km/h (70 mph). Shortly thereafter, due to remaining in almost the same area for hours, Aere began to weaken to a tropical storm, and on October 10, it weakened to a tropical depression, before weakening to a low-pressure area late on October 11. On October 13, Aere re-generated into a tropical depression and it made landfall in Huế, Vietnam late that day. The system moved towards Laos and Thailand before it fully dissipated on October 14.
Typhoon Cary, known as Typhoon Ising in the Philippines, was the second of two tropical cyclones to affect Vietnam in a week. An area of disturbed weather developed southwest of Pohnpei on August 6, 1987. The system initially remained disorganized, but by August 14, Cary had attained tropical storm intensity. After initially moving north-northwest, Cary turned west-northwest, although intensification was slow to occur. On August 15, Cary was upgraded into a typhoon, and on August 17, the typhoon peaked in intensity. Typhoon Cary then made landfall in northern Luzon while at peak intensity. Across the Philippines, 954 houses were damaged and an additional 89 were destroyed, which left 55,567 people, or 13,247 families that were either homeless or otherwise sought shelter. Five people died in the country while damage totaled $5.58 million (1987 USD), including $1.45 million from agriculture and $4.13 million from infrastructure. The storm weakened over land, but re-intensified into a typhoon over the South China Sea. On August 21, Typhoon Cary passed just south of Hainan, where hundreds of homes were damaged but no fatalities occurred, and subsequently entered the Gulf of Tonkin. The storm weakened as it approached Vietnam, and on August 23, the storm dissipated inland over Laos. Across Vietnam, almost 40,000 ha of land were flooded or destroyed. Twenty people were killed and many others were injured.
Typhoon Joe, known in the Philippines as Typhoon Nitang, affected the Philippines, China, and Vietnam during July 1980. An area of disturbed weather formed near the Caroline Islands on July 14. Shower activity gradually became better organized, and two days later, the system was upgraded into a tropical depression. On July 18, the depression was classified as Tropical Storm Joe. Initially, Joe moved northwest, but began to turn to the west-northwest, anchored by a subtropical ridge to its north. Joe started to deepen at a faster clip, and attained typhoon intensity on July 19. The eye began to clear out, and the next day, Joe reached its highest intensity. Shortly thereafter, Joe moved ashore the Philippines. There, 31 people were killed and 300,000 others were directly affected. Around 5,000 homes were destroyed, resulting in an additional 29,000 homeless. Damage in the nation was estimated at $14.5 million (1980 USD).
Typhoon Faith, known in the Philippines as Typhoon Norming, struck both the Philippines and Vietnam during December 1998. A tropical disturbance developed within the vicinity of the western Caroline Islands during early December. At midday on December 8, the system developed into a tropical depression. Tracking northwest at a brisk pace, the depression gradually intensified, and was upgraded into a tropical storm at noon on December 9. Quickly intensifying, Faith turned to the west-northwest, and after tracking near Samar Island on the evening of December 10, Faith attained typhoon intensity. After clipping the northern tip of Palawan Island, the typhoon entered the South China Sea at peak intensity. Across the Philippines, 33 people were killed, with 30 others wounded and 36 others listed missing. A total of 6,423 homes were damaged and 3,234 houses were destroyed, leaving more than 20,000 homeless. Damage was estimated at $25.9 million, with $6.82 million from crops, $15.9 million from public infrastructure, and $3.37 million from private infrastructure.
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