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Severe Tropical Storm Linfa was the second named storm to develop in the South China Sea during the 2009 Pacific typhoon season. It is the seventh depression and third typhoon of the season. Forming out of an area of low pressure on June 14, the storm briefly attained tropical depression status before degenerating. By June 17 the system regenerated in the South China Sea. Slowly tracking northward, the storm intensified, attaining severe tropical storm status on June 19 and peaking in intensity the following day. On June 21, Linfa made landfall in Fujian Province, China as a tropical storm before weakening to a tropical depression. In Taiwan, outer bands of the storm produced significant amounts of rain over southeastern areas of the island. Along the western coast, rip currents resulted in the drowning of one person. Six hikers also were reported to be missing. In China, torrential rains triggered flooding that destroyed 100 homes, killed one person and left six others missing. In all, seven people were killed by Linfa, with damages in mainland China estimated at ¥641 million (US$93.8 million) and agricultural losses in Taiwan reached NT$400 million (US$12.1 million). ==Meteorological history== On June 10, the Joint Typhoon Warning Center (JTWC) began monitoring a persistent area of convection situated about 140 kilometres (85 mi) southeast of Palau. Satellite imagery depicted an elongated low-level circulation with deep convection centered along the southwestern portion of the system. Strong wind shear, which normally inhibits cyclonic development, provided energy for further convective development around the system. Tracking in a general northwestward direction, the low gradually developed northward outflow due to a tropical upper tropospheric trough (TUTT) located north of the disturbance. Following further development, the Japan Meteorological Agency declared the system as a tropical depression at 0600 UTC on June 14. Later on June 14, the JTWC issued a Tropical Cyclone Formation Alert (TCFA) for the depression. Deep convection consolidated around the center of circulation and convective banding features developed along the periphery of the system. Several hours later, the TCFA was canceled as the system rapidly degenerated, with convection mostly dissipating and an exposed low. Outflow significantly deteriorated as the system detached itself from the TUTT. By this time, the JMA had ceased advisories on the depression. Two days later, after tracking across Luzon, the system began to regenerate. Convection redeveloped around the low and outflow was reestablished to the south. Early on June 17, the JTWC issued a second TCFA as the system continued to organize. By this time the system was nearly stationary and at 0600 UTC, the JMA declared that the low had developed into a tropical depression. Several hours later, the JTWC designated the system as Tropical Depression 03W while the storm was situated about 705 km (440 mi) south-southwest of Kaohsiung, Taiwan. Little movement took place for the first few days of the storm's existence as weak steering currents were in place over the South China Sea. Following further development of the depression, the JTWC upgraded it to a tropical storm late on June 17. At 0600 UTC on June 18, the JMA classified the system as a tropical storm and gave it the name ''Linfa''. Limited poleward outflow hindered intensification for the remainder of June 18. By this time, the storm began to increase in forward motion due to a strengthening subtropical ridge located east of Taiwan and a mid-latitude trough to the west. Around 1200 UTC the following day, Linfa further intensified into a severe tropical storm. A microwave satellite image of the storm depicted an eye-feature surrounded by deep convection. Interacting with a nearby upper-level low, poleward outflow significantly improved late on June 19, fueling further strengthening. Slowly tracking in a general northward direction, Linfa continued to organize and by June 20, the JTWC upgraded Linfa to a typhoon. A small, ragged eye appeared on visible satellite images by this time and several hours later, the storm reached its peak intensity just below typhoon-status according to the JMA. Maximum sustained winds peaked at 110 km/h (70 mph 10-minute winds) and a barometric pressure of 975 hPa (mbar). Later on June 20, convection near the center of circulation began to decrease–an indication of weakening–and the eye was no longer visible. Upper-level wind shear rapidly increased to 55 km/h (35 mph), preventing re-intensification of the cyclone. Taking a more northward track than anticipated, Linfa began to interact with land and was downgraded to a tropical storm by the JTWC on June 21. Around 1230 UTC, the storm made landfall in southern Fujian as a tropical storm with winds of 85 km/h (50 mph 10-minute winds). Deep convection rapidly dissipated shortly thereafter due to interaction with land. Several hours later, the JTWC downgraded Linfa to a tropical depression. The following day, the JMA also downgraded Linfa to a tropical depression as the storm moved away from the Chinese coastline. The system later dissipated just offshore; a circulation was no longer evident on satellite imagery. 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 Linfa (2009)」の詳細全文を読む スポンサード リンク
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