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Severe Tropical Storm Koni, known in the Philippines as Tropical Storm Gilas,〔 caused moderate damage to areas of China and Vietnam in July 2003. The eighth tropical storm in the western Pacific that year, Koni originated from a disturbance situated within the monsoon trough well east of the Philippines on July 15. Tracking westward, intensification was slow and the system remained a tropical depression as it moved across the central Philippines on July 17. Upon moving into the South China Sea, however, conditions allowed for quicker strengthening, and as such the cyclone reached tropical storm status on July 18 before reaching its peak intensity with maximum sustained winds of 110 km/h (70 mph) and a minimum barometric pressure of 975 mbar (hPa; 28.79 inHg), making it a severe tropical storm. However, atmospheric conditions began to deteriorate as Koni made landfall on Hainan on July 21, weakening the system. The tropical storm continued to weaken as it moved over the Gulf of Tonkin prior to a final landfall near Hanoi, Vietnam the following day. Tracking inland, the combination of land interaction and wind shear caused Koni to dissipate over Laos on July 23. Shortly after development Koni tracked through the Philippines, killing two people. After moving into the South China Sea, turbulence produced by the storm resulted in an aviation incident involving a commercial airliner off the western Philippines. Three of the plane's occupants received minor injuries. In Hainan, Koni caused heavy rainfall, peaking at 189 mm (7.44 in) at a station on Wuzhi Mountain. The rains resulted in the collapse of 1,400 homes and an estimated CN¥140.27 million (US$16.9 million) in direct economic losses. Effects were worst in Vietnam, where three people were killed. Widespread power outages occurred, and strong winds resulted in agricultural and infrastructural damage, particularly in Vietnam's northern provinces. ==Meteorological history== The precursor to Koni developed as an area of deep convection within an active monsoon trough well south of Guam on July 12. Though atmospheric conditions were favorable for tropical cyclogenesis, the tropical disturbance failed to maintain consistent shower activity. Late on July 14, however, the system developed organized rainbands. This prompted the Japan Meteorological Agency (JMA) to classify the system as a tropical depression at 0000 UTC on July 15, well north of Palau. Shortly after, the storm entered the area of responsibility of the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA), immediately classifying the system as a tropical depression and designating it with the name ''Gilas''; the JTWC later classified the system as such at 1200 UTC that day. A subtropical ridge to the north steered the depression westward for much of its initial stages. On July 16, the JTWC upgraded the system to tropical storm strength,〔 while the JMA maintained the system's tropical depression classification.〔 Through July 17, the tropical cyclone began to track across the central Philippines and concurrently entered hostile atmospheric conditions as wind shear and a suppressed outflow pattern began to impact the storm.〔 However, the cyclone was only a slightly weakened system by the time it emerged into the South China Sea the following day. At the same time, a shortwave trough began to force the storm northwestward towards China. At 0600 UTC on July 18, the JMA upgraded the cyclone to tropical storm status, designating it with the name ''Koni''.〔 Though conditions were more favorable over the South China Sea than over the Philippines, persistent, moderate wind shear prevented much strengthening.〔 However, a brief period of favorable conditions allowed for Koni to strengthen, and at 0000 UTC on July 20 the tropical storm was upgraded to severe tropical storm status by the JMA.〔 Meanwhile, the JTWC upgraded the system to typhoon intensity six hours later.〔 Midday on July 20 Koni began to develop a partial eye.〔 This indicated an increase in intensity, and as such Koni reached a peak in strength at 1800 UTC that day with maximum sustained winds of 110 km/h (70 mph) and a minimum barometric pressure of 975 mbar (hPa; 28.79 inHg). This intensity was maintained for roughly six hours, during which time Koni began to curve westward.〔 However, moderate wind shear conditions returned the following day, weakening the tropical cyclone.〔 At around 1200 UTC on July 21, Koni made landfall on the southeastern coast of Hainan with winds of 95 km/h (60 mph).〔 Land interaction further weakened Koni, and the restrengthening of the subtropical ridge to the cyclone's north resulted in a more westerly path.〔 After a brief reemergence into the Gulf of Tonkin, the system made another landfall, this time south of Hanoi, Vietnam at 0800 UTC on July 22. At this landfall Koni was only estimated to have winds of 85 km/h (50 mph). Upon tracking inland, the storm began to quickly weaken, and was downgraded to tropical depression intensity at 1800 UTC that day over northern Laos. Six hours later, the JMA declared Koni to have dissipated over the same general region.〔 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「Tropical Storm Koni」の詳細全文を読む スポンサード リンク
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