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Tropical Storm Rumbia, known in the Philippines as Tropical Storm Toyang, brought deadly flooding to the central and southern Philippines in November and December 2000. The last of three consecutive tropical cyclones of at least tropical storm intensity to strike the Philippines, Rumbia began as a tropical depression on November 27, gradually intensifying to reach tropical storm intensity the next day. Strengthening later stagnated, and Rumbia would weaken back to depression status as it made landfall on the central Philippines on November 30. Though the Japan Meteorological Agency (JMA) determined Rumbia to have dissipated on December 2, the Joint Typhoon Warning Center (JTWC) continued to monitor the system over the next few days as it tracked across the South China Sea. For a period of time beginning on December 5, Rumbia reorganized and strengthened back to tropical storm intensity before wind shear began to weaken the system. Located south of Vietnam on December 7, the storm's circulation center became devoid of convection, and by then Rumbia was declared by the JTWC to have dissipated. In the Philippines, Rumbia caused roughly US$1 million in damage and 48 fatalities. Several transportation routes were suspended in the lead-up to the storm's landfall. As a result of the tropical storm, power outages occurred, especially in Surigao. Several towns and villages were flooding, displacing around 70,000 people and putting 4,100 people into temporary emergency sheltering. ==Meteorological history== The predecessor to Rumbia developed as an area of convection on November 25, southeast of Palau. The region of disturbed weather was connected with a weak low-pressure area. Embedded within the monsoon trough and tracking westward, the system organized, and as a result the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) designated the storm as Tropical Depression ''Toyang'' at 0000 UTC on November 25. Six hours later, the PAGASA upgraded Toyang to tropical storm status, though at the same time the JMA designated the system as a tropical depression. Despite its cyclogenesis, Toyang maintained monsoonal characteristics for a prolonged period of time. At 1800 UTC on November 28, the Japan Meteorological Agency (JMA) officially upgraded the cyclone to tropical storm status;〔 the system's official name–Rumbia–was designated at that time.〔 Upon attaining tropical storm status, Rumbia was determined to have officially reached its peak intensity, with maximum sustained winds of 75 km/h (45 mph) and a minimum barometric pressure of 990 mbar (hPa; 29.23 inHg).〔 Concurrently, Rumbia's convection strengthened and increased in areal coverage, though persistent wind shear displaced much of the convection west of the circulation center.〔 At 1800 UTC on November 30, the JMA weakened the system to tropical depression status; at the same time Rumbia made landfall over the Central Philippines. Rumbia gradually weakened as it tracked across the archipelago, and on November 1 the depression became quasi-stationary for a transient period of time in the Tablas Strait. The following day, Rumbia entered the South China Sea as a highly diffused system.〔 At 0600 UTC on December 2, the JMA declared Rumbia to have dissipated,〔 while the Joint Typhoon Warning Center (JTWC) continued to monitor the system as an active tropical cyclone.〔 Nonetheless, Rumbia remained highly disorganized, with multiple low-level circulation centers. Over the next few days, as the cyclone continued to track in a general westward direction, persistent inhibiting factors including the entrainment of cold air and wind shear prevented Rumbia from redeveloping. As a result, the depression was anticipated to gradually weaken until dissipation. On December 5, however, the cyclone moved into a favorable position under the axis of an upper-level ridge, allowing for Rumbia to intensify and regain tropical storm intensity at 1200 UTC while located 835 km (520 mi) southeast of Da Nang, Vietnam;〔 despite the recent strengthening the JMA still considered the storm to have already dissipated.〔 This period of strengthening was only temporary, as shearing conditions once again arose, weakening the system and thus resulting in its subsequent downgrade to tropical depression status late the following day. By December 7, Rumbia's main circulation center had become devoid of convection,〔 and the JTWC issued their final warning on the system while the depression was located south of 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「Tropical Storm Rumbia (2000)」の詳細全文を読む スポンサード リンク
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