海洋通报(英文版)
海洋通報(英文版)
해양통보(영문판)
MARINE SCIENCE BULLETIN
2014年
1期
2-14
,共13页
陈波%董德信%陈宪云%刘晖%邱绍芳
陳波%董德信%陳憲雲%劉暉%邱紹芳
진파%동덕신%진헌운%류휘%구소방
广西沿海%热带气旋%灾害成因%影响分析
廣西沿海%熱帶氣鏇%災害成因%影響分析
엄서연해%열대기선%재해성인%영향분석
Guangxi coast%tropical cyclone%disaster causation%impact analysis
登陆或经过广西沿海的热带气旋是一种严重的自然灾害,每年热带气旋所伴随的大风、大雨、风暴潮等灾害造成沿海地区严重的财产损失或人员伤亡。通过对1950~2012年影响广西沿海的热带气旋的统计分析发现,影响广西沿海的热带气旋数量年际变化明显,最多的年份达9个,最少的年份为0个;热带气旋季节分布具有明显规律性,每年的7、8、9三个月为影响高峰月,其次为6、10月;热带气旋从菲律宾以东洋面进入南海后穿过海南省和雷州半岛再次登陆广西沿海的次数最多,该类热带气旋引起的风暴增水平均值为111.2 cm,到达非登陆台风增水的2.6倍。风暴潮灾害的形成与强台风天气系统、全日大潮、河流下泄洪水直接有关。强台风产生巨浪及降雨,使入海河口水位上升,与风暴潮叠加后产生明显的增水,造成巨大的潮灾。
登陸或經過廣西沿海的熱帶氣鏇是一種嚴重的自然災害,每年熱帶氣鏇所伴隨的大風、大雨、風暴潮等災害造成沿海地區嚴重的財產損失或人員傷亡。通過對1950~2012年影響廣西沿海的熱帶氣鏇的統計分析髮現,影響廣西沿海的熱帶氣鏇數量年際變化明顯,最多的年份達9箇,最少的年份為0箇;熱帶氣鏇季節分佈具有明顯規律性,每年的7、8、9三箇月為影響高峰月,其次為6、10月;熱帶氣鏇從菲律賓以東洋麵進入南海後穿過海南省和雷州半島再次登陸廣西沿海的次數最多,該類熱帶氣鏇引起的風暴增水平均值為111.2 cm,到達非登陸檯風增水的2.6倍。風暴潮災害的形成與彊檯風天氣繫統、全日大潮、河流下洩洪水直接有關。彊檯風產生巨浪及降雨,使入海河口水位上升,與風暴潮疊加後產生明顯的增水,造成巨大的潮災。
등륙혹경과엄서연해적열대기선시일충엄중적자연재해,매년열대기선소반수적대풍、대우、풍폭조등재해조성연해지구엄중적재산손실혹인원상망。통과대1950~2012년영향엄서연해적열대기선적통계분석발현,영향엄서연해적열대기선수량년제변화명현,최다적년빈체9개,최소적년빈위0개;열대기선계절분포구유명현규률성,매년적7、8、9삼개월위영향고봉월,기차위6、10월;열대기선종비률빈이동양면진입남해후천과해남성화뇌주반도재차등륙엄서연해적차수최다,해류열대기선인기적풍폭증수평균치위111.2 cm,도체비등륙태풍증수적2.6배。풍폭조재해적형성여강태풍천기계통、전일대조、하류하설홍수직접유관。강태풍산생거랑급강우,사입해하구수위상승,여풍폭조첩가후산생명현적증수,조성거대적조재。
The tropical cyclone that lands or passes through Guangxi coast is a serious natural disaster, which brings about strong winds, heavy rains, storm surges and other disasters causing severe damage of property or casualties in the coastal region every year. By counting and analyzing the tropical cyclones affecting Guangxi coast from 1950 to 2012, we find that the annual number of tropical cyclones changes significantly, and the maximum value can be up to 9, whereas the minimum value is 0 in some year. The regularity of seasonal distribution of tropical cyclones is obvious, and the peak period is in July, August and September every year, followed by June and October. Most of tropical cyclones come from the east of Philippines. After entering the South China Sea and passing through Hainan province and Leizhou Peninsula, they landed on Guangxi coast once again and caused the mean of peak surge reaching 111.2 cm, which is 2.6 times of non-landing typhoon. The formation of storm surge disaster is directly related to the severe typhoon weather systems, diurnal spring tide and discharge of river flood. Severe typhoons generate huge waves and rainfal , which lead to the rise of water level at the estuary, and would result in significant increasing water when stacking up with the storm surge, and cause huge tidal disaster.