Meteorological history | |
---|---|
Formed | August 4,2007 |
Dissipated | August 10,2007 |
Typhoon | |
10-minute sustained (JMA) | |
Highest winds | 120 km/h (75 mph) |
Lowest pressure | 975 hPa (mbar);28.79 inHg |
Category 1-equivalent typhoon | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 130 km/h (80 mph) |
Lowest pressure | 970 hPa (mbar);28.64 inHg |
Overall effects | |
Fatalities | 15 |
Missing | 1 |
Damage | $227 million (2007 USD) |
Areas affected | Philippines,Taiwan,and China |
IBTrACS | |
Part of the 2007 Pacific typhoon season |
Typhoon Pabuk,known in the Philippines as Tropical Storm Chedeng,was a minimal typhoon that formed on August 5,2007. The system made landfall on Taiwan on August 7,and on August 9 Pabuk passed to the south of Hong Kong. [1]
On August 4, the Japan Meteorological Agency began monitoring a tropical depression. [1] [ clarification needed ] The system continued to strengthen, and the Joint Typhoon Warning Center issued a Tropical Cyclone Formation Alert on the system early the next day, noting that its environment was "strongly favorable for development". [2] The Japan Meteorological Agency designated the system Tropical Storm Pabuk shortly after. [3] The JTWC designated the system Tropical Storm 07W at about the same time, and on August 5 PAGASA named the system Chedeng. As Pabuk continued to move to the northwest, it gained some organisation as it slowly developed outflow. [4] It was upgraded by the JMA to a severe tropical storm on August 6. Moving westwards towards Taiwan, an area of convection south of Pabuk separated and formed its own low-level circulation. Pabuk's upper-level outflow inhibited this new area of convection. Strengthening slightly, Pabuk was upgraded to a typhoon on the morning of August 7. The JTWC downgraded Pabuk to a tropical storm later that day, with the JMA downgrading Pabuk shortly before landfall. It made landfall in southern Taiwan around 1630 UTC according to Taiwan radar and crossed the southern tip of the Hengchun Peninsula in Pingtung County. The JTWC re-upgraded Pabuk to a typhoon at its next advisory, however, citing a small eye at landfall, [5] before downgrading it to a tropical storm again three hours later. [6]
After passing over Taiwan, Pabuk took aim at Hong Kong. [7] On August 9 as the system passed to the south of Hong Kong JMA downgraded the storm to a tropical depression later that day and issued its final public advisory, with the JTWC following suit shortly after. The tropical depression then turned back to the east-northeast on August 10, [8] intensifying while taking aim at Hong Kong. It skirted to the west of Hong Kong and dissipated while heading northeast into the mainland.
Authorities in Manila closed all schools and government offices on August 8 as the outer bands of Pabuk triggered deadly flooding and landslides. [9] On August 7, Taiwanese authorities issued land and sea warnings for most of the island as Typhoon Pabuk was expected to make landfall the following day. [10] Government officials in Taiwan stockpiled nearly 6,000 sandbags to quickly respond to any flood disasters and cleanup crews were rushed into cities to clear gutters and storm drains in advance of heavy rain. Shopkeepers were advised not to tighten billboards to avoid harming others. [11]
As Pabuk made landfall in southern Taiwan on August 8, Chinese officials evacuated an estimated 20,000 residents from coastal areas in Fujian Province. Roughly 6,700 vessels were also called back to port in anticipation of rough seas. [12] An estimated 1.7 million text messages were also sent out to inform the public about the storm. [13]
The Hong Kong Observatory (HKO) and Macau's Meteorological and Geophysical Bureau (SMG) both hoisted Strong Wind Signal No. 3 on August 9 as the system passed to the south of Hong Kong, they were canceled later. On August 10 the signals were re-issued as the tropical storm looped and turned northeast. The HKO also warned that winds were expected to strengthen further locally, and that the Hong Kong Education Bureau had suspended all classes for the day. [14] After upgrading Pabuk to a tropical storm, [15] the HKO issued the No. 8 Southwest Gale or Storm Signal at 2:30 p.m. HKT (0630 UTC) later that day as Pabuk reached the closest point of approach to the Hong Kong Observatory Headquarters (skirting at 30 km west-northwest of the HKO Headquarters), and was about to make landfall near Lung Kwu Tan, Tuen Mun. [16] This was replaced by signal 3 later while Pabuk took another turn in direction and headed west inland into Guangdong. Early next morning, Pabuk resumed a northeasterly track, edging once again closer to the Pearl River Delta [17] before it weakened further and HKO cancelled all signals. [18]
As Pabuk neared Taiwan, the outer rainbands from the storm triggered monsoon rains over the northern Philippines, causing numerous landslides. In the mining town of Maco in Compostela Valley, seven houses were buried under mud, leaving ten people dead. Farther north, another person, a young boy, was killed by a landslide. [19] The streets of Manila were flooded by rains which left low-lying areas under neck-deep waters. [20] The rains also led to the collapse of a concrete wall, burying five children. Firefighters quickly rushed to the building and pulled the children out, all of them only sustained minor injuries. [21] After Pabuk struck Taiwan, another storm, Tropical Storm Wutip, brought more rains to the Philippines. The combined fatalities from the two storms totaled to 15, left one person missing, and injured ten others. About 1.2 million people were affected by the two storms and damages were estimated at $6.8 million (2007 USD). [22]
Despite being a typhoon upon making landfall near Eluanbi in southern Taiwan, Pabuk caused little damage. [19] Near where the typhoon made landfall, weather radar estimated that the area received rainfall in excess of 305 mm (12 in). [23] The heavy rains helped alleviate severe drought conditions which had persisted in southern Taiwan for several months. [24] At its peak, 60,000 residences were without power. No fatalities were caused by the storm and only $200,000 (2007 USD) was left in farm damages. [25]
Record setting rains fell in southern China as Pabuk stalled near Hong Kong. Zhanjiang, near the island of Hainan, recorded a 24‑hour rainfall measurement of 739 mm (29.1 in), higher than any other single day event in the past 200 years. Numerous stretches of highways and railways were damaged by the floods that followed. Several trains were cancelled due to the washed out tracks. Two dams reached record water levels and five dams reached the water danger mark. The Dawan Reservoir nearly overflowed, but workers dug canals around it to release the excess water in a controlled manner. [26] The storm left 64,200 people homeless, affected over 1.1 million, and about 4,200 homes were destroyed. Damages from Pabuk were estimated at $220 million (2007 USD). [27]
Despite the torrential rains, there were no reports of any fatalities associated with the storm. [26]
A storm surge of 0.45 m (1.47 ft) was recorded in Hong Kong. [28] On August 10, during the storm's second pass by Hong Kong, maximum 10-minute mean wind reached 101 km/h (which is storm-force) on Cheung Chau right before the issuance of No. 8 Southwest Gale or Storm Signal, and wind gust reaching 122 km/h (66 kt) was recorded on Ngong Ping (which is a high ground) at 7:16PM local time (11:16AM UTC), despite Pabuk only being a tropical storm. [29]
The 2005 Pacific typhoon season was the least active typhoon season since 2000, producing 23 named storms, of which 13 became 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 2005, though most tropical cyclones typically develop between May and October. The season's first named storm, Kulap, developed on January 13, while the season's last named storm, Bolaven, dissipated on November 20. The season's first typhoon, Haitang, reached typhoon status on July 13, and became the first super typhoon of the year three days later.
The 2006 Pacific typhoon season was a near-average season which produced a total of 23 named storms, 15 typhoons, and six super typhoons. The season ran throughout 2006, though most tropical cyclones typically develop between May and October. The season's first named storm, Chanchu, developed on May 9, while the season's last named storm, Trami, dissipated on December 20.
The 2007 Pacific typhoon season was a near average season which featured 24 named storms, fourteen typhoons, and five 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 2007, though most tropical cyclones typically develop between May and November. The season's first named storm, Kong-rey, developed on March 30, while the season's last named storm, Mitag, dissipated on November 27. The season's first typhoon, Yutu, reached typhoon status on May 18, and became the first super typhoon of the year on the next day.
The 2001 Pacific typhoon season was an average season with twenty-six named storms, sixteen typhoons and three super typhoons, with a near normal Accumulated Cyclone Energy (ACE) of 307.3 units. It ran year-round in 2001, with most tropical cyclones in the northwestern Pacific Ocean tending between May and November.
This timeline documents all events that have taken place during the 2007 Pacific typhoon season. This article is limited to the Western Pacific basin which is located north of the equator and between 100°E and the International Date Line. Systems that reach tropical storm intensity are assigned a name by the Japan Meteorological Agency (JMA). Tropical depressions that form within the basin are assigned a number with a "W" suffix by the Joint Typhoon Warning Center (JTWC). Additionally, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that either form in or move into its self defined area of responsibility, which runs from 135°E to 115°E and 5°N to 25°N.
The 2008 Pacific typhoon season was a below average season which featured 22 named storms, eleven typhoons, and two super typhoons. The season had no official bounds; it ran year-round in 2008, but 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.
Super Typhoon Kent, known in the Philippines as Typhoon Gening, was a powerful Category 4-equivalent typhoon that formed in late August during the 1995 Pacific typhoon season.
Typhoon Sepat, known in the Philippines as Super Typhoon Egay, was the eighth named tropical storm and the strongest tropical cyclone of the 2007 Pacific typhoon season, that affected the Philippines and made landfall in Taiwan and Fujian. Sepat originated on August 11 via a low-circulation center SE of Naha, Okinawa, and was named by the Japan Meteorological Agency as Sepat on August 12 and Egay in the Philippines by PAGASA as it entered the PAR. Sepat underwent an explosive intensification on the night of August 13, reaching peak intensity at Category 5-equivalent super typhoon intensity the following morning. The storm maintained its strength for 2 days, until it underwent an eyewall replacement cycle, just before he storm makes landfall in Taiwan on August 17 as a Category 3-equivalent typhoon. After crossing the Taiwanese strait, Sepat; already weakening into Category 1 status due to unfavorable conditions, made a second landfall in China on August 18, 2007. The storm persisted across Mainland China, as it transitioned into an extratropical cyclone on August 20, and Sepat, now an extratropical low continued through the Chinese mainland until it finally dissipated near Yunnan Province on August 24.
Typhoon Fengshen, known in the Philippines as Typhoon Frank, was the sixth named storm and the fourth typhoon recognized by the Japan Meteorological Agency. The Joint Typhoon Warning Center recognized Fengshen as the seventh tropical depression, the sixth tropical storm, and fifth typhoon of the 2008 Pacific typhoon season.
Severe Tropical Storm Kammuri, known in the Philippines as Tropical Storm Julian, was a weak but deadly tropical storm which impacted the Philippines, China, Vietnam, and Hong Kong in August 2008. The ninth named storm of the 2008 Pacific typhoon season, Kammuri developed as a tropical depression on August 4 north of Luzon. The next day, the depression intensified into a tropical storm, resulting in the Japan Meteorological Agency naming it Kammuri. The following day, Kammuri reached its peak intensity with sustained winds of 50 kn (93 km/h) before making landfall in Guangdong province, China. This would make Kammuri weaken into a tropical storm that evening, resulting in the JTWC issuing their last advisory on the system. Kammuri would later emerge in the Gulf of Tonkin the next day, making a second landfall over Guangxi province, China. After Kammuri made landfall, the JMA issued its final advisory on Kammuri.
Typhoon Nuri, known in the Philippines as Typhoon Karen, was the 12th named storm and the seventh typhoon that was recognised by the Japan Meteorological Agency. The Joint Typhoon Warning Center recognised it as the 13th tropical depression, the 12th tropical storm and the 8th typhoon of the 2008 Pacific typhoon season. The name Nuri was submitted to the World Meteorological Organisation's Typhoon Committee by Malaysia in 2003 after the name Rusa was retired in 2002. The name Nuri is Malay for a blue crowned parroquet, a type of parrot. The name Karen was assigned by PAGASA to a tropical depression for the second time, the other time being in 2004 to Typhoon Rananim.
Typhoon Hagupit, known in the Philippines as Typhoon Nina, was a powerful cyclone that caused widespread destruction along its path in September 2008. The 21st depression, 14 tropical storm and 10th typhoon of the 2008 Pacific typhoon season, Hagupit developed from a tropical wave located a couple hundred miles east of the Marshall Islands on September 14. Moving generally north-west westwards towards the Philippines, the depression gradually intensified into a tropical storm the following day, and then into became a typhoon on September 22 off the northern coast of Luzon. Located within an environment conducive for strengthening, Hagupit rapidly strengthened to attain 10-min sustained winds of 165 kilometres per hour and 1-min sustained winds of 230 kilometres per hour. After making landfall in Guangdong province in China at peak intensity on September 23, Hagupit rapidly weakened over rugged terrain and dissipated on the 25th.
Typhoon Prapiroon, known in the Philippines as Tropical Storm Henry, was a minimal typhoon which caused deadly flooding in southern China in August 2006. Prapiroon developed out of a persistent area of convection accompanied by an area of low pressure on July 25 about 120 km (75 mi) west-southwest of Yap. Two days later, both the Japan Meteorological Agency (JMA) and PAGASA classified the system as a tropical depression, with PAGASA giving it the local name 'Henry'. By July 31, the Joint Typhoon Warning Center (JTWC) classified the system as Tropical Depression 07W. A strong subtropical ridge located to the north of the depression led to a west-northwest movement for most of the storm existence.
Typhoon Conson, known in the Philippines as Typhoon Frank, was the first of the record ten typhoons to impact Japan during the 2004 Pacific typhoon season. Developing out of a tropical depression near the northern Philippines in early June, Conson slowly traveled towards the north. Gradually strengthening, the storm reached typhoon status late on June 7 according to the Joint Typhoon Warning Center and several hours later according to the Japan Meteorological Agency. After turning towards the northeast, the typhoon brushed Taiwan and reached its peak intensity with 10-minute sustained winds of 150 km/h (90 mph) on June 9. After reaching its peak, Conson gradually weakened, passing through Okinawa before being downgraded to a tropical storm the next day. On June 11, the storm made landfall as a minimal tropical storm in the Kōchi Prefecture just before becoming extratropical. The extratropical remnants continued towards the northeast and were last mentioned on June 14 crossing the International Date Line.
Typhoon Andy, known in the Philippines as Typhoon Iliang, was an intense tropical cyclone that made landfall in Taiwan. Andy formed along the northern edge of the monsoon trough south of Guam on July 22, 1982. It became a tropical storm the next day, although this system was initially poorly organized. Andy moved steadily west during the first few days of its life. After looping south of Guam, the cyclone moved northwest and strengthened. Andy turned westward near the 18th parallel on July 25. The system became a strong typhoon for a prolonged period on July 27 and July 28 while attaining a peak intensity of 185 km/h (115 mph). However, the typhoon struck Southern Taiwan on July 29. Continuing westward through the Formosa Strait, the storm made its final landfall in southern China on July 30 and dissipated inland two days later.
Typhoon Vicente, known in the Philippines as Tropical Depression Ferdie, was the strongest tropical cyclone to strike the Chinese province of Guangdong since Hagupit in 2008, and was regarded as the strongest storm to affect Hong Kong and Macau in more than ten years. The eighth named storm and third typhoon of the 2012 Pacific typhoon season, Vicente began as a tropical depression on July 18, 2012 northeast of the Philippines. Vicente soon steadily moved into the South China Sea, and began to intensify above warm sea waters, and began explosive intensification early on July 23, and started to charge toward the Guangdong region prompting the Hong Kong Observatory (HKO) to issue the Hurricane Signal, No. 10, the first since York in 1999. The Macao Meteorological and Geophysical Bureau also hoisted Signal No. 9 for the first time since York and after the transfer of sovereignty over Macau. Late on the same day, Vicente made landfall over Taishan in Guangdong, China.
Severe Tropical Storm Rumbia, known in the Philippines as Tropical Storm Gorio, was a tropical cyclone that brought widespread flooding in areas of the Philippines and China late June and early July 2013. The sixth internationally named storm of the season, Rumbia formed from a broad area of low pressure situated in the southern Philippine Sea on June 27. Steadily organizing, the initial tropical depression moved towards the northwest as the result of a nearby subtropical ridge. On June 28, the disturbance strengthened to tropical storm strength, and subsequently made its first landfall on Eastern Samar in the Philippines early the following day. Rumbia spent roughly a day moving across the archipelago before emerging into the South China Sea. Over open waters, Rumbia resumed strengthening, and reached its peak intensity with winds of 95 km/h (50 mph) on July 1, ranking it as a severe tropical storm. The tropical cyclone weakened slightly before moving ashore the Leizhou Peninsula late that day. Due to land interaction, Rumbia quickly weakened into a low pressure area on July 2 and eventually dissipated soon afterwards.
Tropical Storm Morakot, known in the Philippines as Tropical Storm Juaning, brought significant rainfall to Taiwan before alleviating drought conditions in mainland China in August 2003. The tenth named storm in the western Pacific that year, Morakot spawned from an area of disturbed weather in the Philippine Sea on July 31. Tracking northwest, favorable conditions allowed for the intensification of the system to tropical storm strength on August 2. Morakot reached peak intensity later that day with winds of 85 km/h (50 mph) and a minimum barometric pressure of 992 mbar. This intensity was held for several hours until less conducive atmospheric conditions slightly weakened the system; this was followed by Morakot making landfall on southern Taiwan on August 3. Subsequently, the storm weakened and moved into the Taiwan Strait before making its final landfall near Quanzhou, China the next day. The storm quickly weakened over the Chinese mainland, and dissipated entirely several hours after landfall.
Tropical Storm Bebinca was a weak but erratic and long-lived tropical cyclone that affected South China and Vietnam in mid-August 2018. Bebinca originated from a tropical depression over the South China Sea on August 9. Maintaining this intensity for a few days near the Guangdong coast, the system intensified into a tropical storm south of Jiangmen on August 13. The storm moved slowly to the east and then curved back on the next day, before making landfall in the Leizhou Peninsula on August 15. Bebinca crossed the Gulf of Tonkin and made landfall in Vietnam on August 16, before dissipated on the next day.
Typhoon Saola, known in the Philippines as Super Typhoon Goring, was a powerful and erratic tropical cyclone that affected the Philippines, southern Taiwan, Hong Kong, Macau and South China. The name Saola, is in reference to a rare animal found in Vietnam. The ninth named storm, seventh typhoon, and third super typhoon of the 2023 typhoon season, Saola originated from an area of convection east of Taiwan and headed southwestwards.
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