About: Tropical Storm Linfa (2003)

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Severe Tropical Storm Linfa, known in the Philippines as Tropical Storm Chedeng, brought deadly flooding to areas of the Philippines and Japan in May and June 2003. The fourth named storm within the northwestern Pacific that year, Linfa developed as a tropical depression just off the western coast of Luzon on May 25. The disturbance quickly intensified to reach tropical storm intensity a few hours after cyclogenesis. However, intensification leveled off as Linfa executed a small clockwise loop before a subsequent landfall on Luzon on May 27. Due to land interaction the storm temporarily weakened and decoupled before reforming in the Philippine Sea. Afterwards Linfa began reintensifying and reached its peak intensity on May 29 with maximum sustained winds of 100 km/h (65 mph) and a barometr

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  • Severe Tropical Storm Linfa, known in the Philippines as Tropical Storm Chedeng, brought deadly flooding to areas of the Philippines and Japan in May and June 2003. The fourth named storm within the northwestern Pacific that year, Linfa developed as a tropical depression just off the western coast of Luzon on May 25. The disturbance quickly intensified to reach tropical storm intensity a few hours after cyclogenesis. However, intensification leveled off as Linfa executed a small clockwise loop before a subsequent landfall on Luzon on May 27. Due to land interaction the storm temporarily weakened and decoupled before reforming in the Philippine Sea. Afterwards Linfa began reintensifying and reached its peak intensity on May 29 with maximum sustained winds of 100 km/h (65 mph) and a barometric pressure of 980 mbar (hPa; 28.94 inHg). Following its peak the tropical storm began to deteriorate and transitioned into an extratropical cyclone on May 30; these extratropical remnants continued to track northward through Japan before dissipating in the Sea of Okhotsk on June 4. The erratic and slow movement of Linfa off the western Philippines was the catalyst for extreme rainfall and flooding, killing 41 persons in the archipelago. Precipitation peaked at 723 mm (28.5 in) near Dagupan. Rising floodwaters resulted in numerous mudslides and the temporary shutdown of government offices. In addition, strong winds caused widespread power outages. Overall damage from Linfa in the Philippines amounted to ₱192.3 million (US$3.65 million). The floods also displaced 8,367 people in 1,686 families and destroyed 178 homes. Linfa and its extratropical remnants later brought torrential rainfall and widespread flooding to Japan, particularly southwestern regions. Rainfall there peaked at 727 mm (28.62 in). Flood damage was worst in Kōchi and Tokushima Prefectures, where several buildings were destroyed by floodwater. Other locations in Japan experienced considerable agricultural damage as well as numerous landslides. Overall, Linfa caused roughly $28.2 million in damage, much of which occurred in Japan, though the entirety of deaths associated with the cyclone took place in the Philippines. (en)
  • 平成15年台風第4号（へいせい15ねんたいふうだい4ごう、アジア名：リンファ/Linfa）は、2003年5月に発生し、日本に上陸した台風である。 (ja)
  • 強烈熱帶風暴蓮花（英語：Severe Tropical Storm Linfa），在菲律賓被稱為熱帶風暴切登，在2003年5月和6月給菲律宾和日本部份地區帶來死傷慘重的水災。當年第四場獲得命名的西北太平洋風暴，蓮花在5月25日於呂宋西岸附近發展成熱帶低氣壓。擾動在後僅數小時便迅速增強，並達到熱帶風暴標準。然而，隨著蓮花在5月27日順時針旋轉一小圈並登陸呂宋，強度趨於平穩。由於與陸地相互作用，風暴在菲律宾海重整前稍為減弱且結構轉差。之後蓮花開始重新增強並在5月29日達到最大持续风速每小時100公里、最低气压980毫巴（百帕；28.94英寸汞柱）的最高強度。在達到最高強度後，熱帶風暴開始減弱，並在5月30日轉變成溫帶氣旋。這些溫帶殘留繼續向北橫越日本，然後在6月4日於鄂霍次克海消散。 蓮花在菲律賓以西的飄忽不定且緩慢移動是導致極端降雨和水災的催化劑，在該島國造成41人死亡。附近的最大降水達到723毫米。不斷上漲的洪水引發大量泥石流，逼使政府辦公室暫時關閉。此外，強風導致大範圍停電。蓮花在菲律造成的整體損失達1.923億披索（365萬美元）。水災還使包括1,686個家庭在內的8,367人流離失所，並摧毀178所房屋。蓮花及其溫帶殘留後來為日本，特別是西南部地區帶來暴雨和大範圍的水災。當地的最高降雨量達到727毫米。高知县和德岛县的水災損失最為嚴重，當地的幾座建築物被洪水摧毀。日本的其餘地方經歷相當大的農業破壞以及多宗山泥傾瀉。整體而言，蓮花造成大約2820萬美元的損失，其中大部分發生在日本，然而全部與氣旋有關的死亡均發生在菲律賓。 (zh)
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  • 平成15年台風第4号（へいせい15ねんたいふうだい4ごう、アジア名：リンファ/Linfa）は、2003年5月に発生し、日本に上陸した台風である。 (ja)
  • Severe Tropical Storm Linfa, known in the Philippines as Tropical Storm Chedeng, brought deadly flooding to areas of the Philippines and Japan in May and June 2003. The fourth named storm within the northwestern Pacific that year, Linfa developed as a tropical depression just off the western coast of Luzon on May 25. The disturbance quickly intensified to reach tropical storm intensity a few hours after cyclogenesis. However, intensification leveled off as Linfa executed a small clockwise loop before a subsequent landfall on Luzon on May 27. Due to land interaction the storm temporarily weakened and decoupled before reforming in the Philippine Sea. Afterwards Linfa began reintensifying and reached its peak intensity on May 29 with maximum sustained winds of 100 km/h (65 mph) and a barometr (en)
  • 強烈熱帶風暴蓮花（英語：Severe Tropical Storm Linfa），在菲律賓被稱為熱帶風暴切登，在2003年5月和6月給菲律宾和日本部份地區帶來死傷慘重的水災。當年第四場獲得命名的西北太平洋風暴，蓮花在5月25日於呂宋西岸附近發展成熱帶低氣壓。擾動在後僅數小時便迅速增強，並達到熱帶風暴標準。然而，隨著蓮花在5月27日順時針旋轉一小圈並登陸呂宋，強度趨於平穩。由於與陸地相互作用，風暴在菲律宾海重整前稍為減弱且結構轉差。之後蓮花開始重新增強並在5月29日達到最大持续风速每小時100公里、最低气压980毫巴（百帕；28.94英寸汞柱）的最高強度。在達到最高強度後，熱帶風暴開始減弱，並在5月30日轉變成溫帶氣旋。這些溫帶殘留繼續向北橫越日本，然後在6月4日於鄂霍次克海消散。 (zh)
rdfs:label
  • 平成15年台風第4号 (ja)
  • Tropical Storm Linfa (2003) (en)
  • 強烈熱帶風暴蓮花 (2003年) (zh)
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