|
Typhoon Imbudo, known in the Philippines as Typhoon Harurot, was a powerful typhoon that struck the Philippines and southern China in July 2003. The seventh named storm and fourth typhoon of the season, Imbudo formed on July 15 to the east of the Philippines. The storm moved generally west-northward for much of its duration due to a ridge to the north. Favorable conditions allowed Imbudo to intensify, gradually at first before undergoing rapid deepening on July 19. After reaching typhoon status, Imbudo strengthened further to peak 10–minute sustained winds of 165 km/h (105 mph) on July 20. The typhoon made landfall on northern Luzon near peak intensity on July 22, but quickly weakened over land. Once in the South China Sea, Imbudo re-intensified slightly before making its final landfall in southern China near Yangjiang on July 24, dissipating the next day. In the Philippines, Imbudo was the strongest typhoon in five years, causing widespread flooding and power outages in the Cagayan Valley for weeks. Damage was heaviest in Isabela province near where the storm struck. Most of the banana crop was destroyed, and other crops sustained similar but lesser damage. Imbudo disrupted transportation across much of Luzon. Nationwide, the storm damaged or destroyed 62,314 houses, causing P4.7 billion (PHP, $86 million USD) in damage, mostly in the Cagayan Valley. There were also 64 deaths in the country. In Hong Kong, strong winds killed a man after knocking him off a platform. In China, damage was heaviest in Guangdong where the storm struck. Thousands of trees fell, and 595,000 houses were wrecked. Hundreds of canceled flights stranded travelers across the region. In Guangxi, high rainfall increased water levels in 45 reservoirs to warning levels. In Guangxi and Guangdong, collectively 20 people were killed, and damage reached about ¥4.45 billion (CNY, $297 million USD). ==Meteorological history== The origins of Imbudo were from a disorganized area of convection near Chuuk in the open western Pacific in mid-July. With weak wind shear, the system slowly became better organized. On July 15, the Japan Meteorological Agency (JMA) estimated that a tropical depression formed.〔 The next day, the Joint Typhoon Warning Center (JTWC) issued a tropical cyclone formation alert (TCFA), noting that outflow had increased due to an upper-level low to the northeast. At 1800 UTC on July 16, the JTWC initiated advisories on Tropical Depression 09W about 665 km (415 mi) east of Yap.〔 A subtropical ridge near Okinawa steered the nascent depression to the west-northwest for much of its duration. With warm waters and favorable upper-level conditions, the depression quickly organized, and the JMA upgraded it to Tropical Storm Imbudo on July 17.〔 After becoming a tropical storm, Imbudo passed about 35 km (20 mi) north of Yap.〔 The JMA upgraded Imbudo to a severe tropical storm late on July 18,〔 around the same time that the JTWC upgraded it to a typhoon. An increase in outflow to the south and to the north from a tropical upper tropospheric trough (TUTT) caused a 36 hour period of rapid development beginning on July 19.〔 During that time, the JMA upgraded Imbudo to typhoon status,〔 the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) began issuing advisories as the storm approached the Philippines,〔 and a 30 km (20 mi) wide eye formed.〔 At 1200 UTC on July 20, the JMA estimated peak 10 minute sustained winds of 165 km/h (105 mph).〔 At the same time, the JTWC estimated 1 minute sustained winds of 240 km/h (150 mph), making it a super typhoon.〔 By late on July 20, the typhoon had developed concentric eyewalls, and the TUTT was moving away, thus diminishing outflow.〔 Imbudo maintained peak winds for about 12 hours,〔 before the innermost eye contracted to a diameter of 11 km (7 mi) in the midst of an eyewall replacement cycle.〔 At 0300 UTC on July 22, Imbudo struck northern Luzon, with 1 minute winds estimated at 205 km/h (125 mph) by the JTWC.〔 Rapidly weakening over land, Imbudo emerged into the South China Sea about six hours after landfall.〔〔 The JTWC estimated winds had decreased to 150 km/h (90 mph), although the agency estimated Imbudo quickly re-intensified to a secondary peak of 165 km/h (105 mph) in 1 minute winds. Dry air prevented convection from redeveloping significantly, and the eye had become large over open waters.〔 At 0300 UTC on July 24, Imbudo made its final landfall west of Macau,〔 near Yangjiang, Guangdong.〔 It was the strongest to hit the province since Typhoon Sally in 1996, striking China with 10 minute winds of 140 km/h (85 mph), as estimated by the JMA. The storm rapidly weakened over land while moving over southern China. Late on July 25, Imbudo dissipated near the border of China and Vietnam.〔 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Typhoon Imbudo」の詳細全文を読む スポンサード リンク
|