Zhang Rongyan, Xu Zonghuan, You Lijun, et al. Wind and rainfall features and risk assessment of tropical cyclone in Fujian. J Appl Meteor Sci, 2012, 23(6): 672-682.
Citation: Zhang Rongyan, Xu Zonghuan, You Lijun, et al. Wind and rainfall features and risk assessment of tropical cyclone in Fujian. J Appl Meteor Sci, 2012, 23(6): 672-682.

Wind and Rainfall Features and Risk Assessment of Tropical Cyclone in Fujian

  • Received Date: 2012-04-16
  • Rev Recd Date: 2012-09-19
  • Publish Date: 2012-12-31
  • Tropical cyclone (TC) influences Fujian Province frequently and often makes severe damages. The damages aroused by TC depend on undertaker, disaster defense abilities and the factors such as environment, weather and so on.The weather factor is a trigger and the essential term of the damage. TCs from 1961 to 2010 which affect Fujian Province are divided into 11 types according to their landing sites and moving paths. Then spatial features of rainfall and wind speed of each TC type are given, and then spatial features of damage potential are given based on them. Evidence shows that TCs landing Fujian Province mostly land Taiwan first and often result in rainfall and strong wind speed, meanwhile TCs landing south to the Pearl River estuary only result in strong wind speed in Fujian Province. The most serious damages aroused by rainfall located in north of Ningde and Jinjiang, while the strongest wind speed occurs in south coastal area of the Province. TCs landing Taiwan and then landing north of the Province again cause the heaviest rainfall, the strongest wind speed aroused by TCs landing Taiwan and then landing south of the Province, TCs landing Taiwan and landing south of the Province again, then landing south of the Province directly cause the broadest area of strong wind speed. Using objective correlation coefficient weighting, an assessment model of damage potential of rainfall and strong wind speed is established. The model reveals some facts: The highest damage potential area is often near the landing site and north to it. When TCs move westward into inland, it often produces a secondly highest area. TCs landing Taiwan, then landing north or middle of the Province again produce the highest damage potential, and landing south of the Province directly or landing south to the Pearl River estuary. High damage potential areas mostly appear in coastal area, west or north of the Province, while low potential areas appear in the river basin.
  • Fig. 1  Diagram of different landing and influencing tropical cyclone paths in Fujian

    Fig. 2  Different path frequency of tropical cyclones landing (a) and influencing (b) Fujian

    Fig. 3  Different path frequency of tropical cyclones according to wind and rain weather

    Fig. 4  The daily maximum precipitation of landing tropical cyclones

    Fig. 5  Daily maximum wind speed of landing tropical cyclones

    Fig. 6  The disaster risk section map of rain and wind index about different landing tropical cyclone paths in Fujian

    Fig. 7  The risk section map of rain and wind index about different influencing tropical cyclone paths in Fujian

    Table  1  Standard of tropical cyclones path classification

    分类 序号 路径 备注
    登陆类 1 直接登陆闽北 从我国台湾北部沿海经过登陆福建沿海,登陆地点包括福建中部和北部
    2 直接登陆闽南 从我国台湾南部沿海经过登陆福建沿海,登陆地点包括福建中部和南部
    3 登台入闽北 先登陆我国台湾,再登陆福州至福鼎 (含福鼎) 沿海
    4 登台入闽中 先登陆我国台湾,再登陆厦门至福州 (含福州) 沿海
    5 登台入闽南 先登陆我国台湾,再登陆诏安至厦门 (含厦门、诏安) 沿海
    影响类 6 登陆珠江口及以东 登陆珠江口 (含珠江口) 及以东至诏安
    7 登陆珠江口以西 登陆珠江口以西,包括广西、海南
    8 登陆浙江及以北 登陆浙江及以北的我国大陆
    9 登陆我国台湾 登陆我国台湾后转向,未在我国大陆登陆
    10 海峡内消失 台湾海峡内消失
    11 海峡外消失 除以上10条路径外的其他路径
    DownLoad: Download CSV
  • [1]
    王维国, 王秀荣, 许映龙, 等.超强台风"桑美"特征及预报服务效益分析.自然灾害学报, 2008, 17(3):106-111. http://www.cnki.com.cn/Article/CJFDTOTAL-ZRZH200803019.htm
    [2]
    林炳荣.近10年福建台风灾害分析.福建地理, 1999, 14(2):21-28. http://www.cnki.com.cn/Article/CJFDTOTAL-FJDL199902004.htm
    [3]
    张丽佳, 刘敏, 陆敏, 等.中国东南沿海地区台风危险性评价.人民长江, 2010, 41(6):81-83. http://www.cnki.com.cn/Article/CJFDTOTAL-RIVE201006022.htm
    [4]
    徐文慧, 倪允琪.登陆台风环流内的一次中尺度强对流过程.应用气象学报, 2009, 20(3):267-275. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20090302&flag=1
    [5]
    张永恒, 范广洲, 马青云, 等.浙江省台风灾害影响评估模型.应用气象学报, 2009, 20(6):772-776. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20090617&flag=1
    [6]
    董林, 端义宏.热带气旋经过台湾岛强度变化特征.气象, 2008, 34(7):10-14. doi:  10.7519/j.issn.1000-0526.2008.07.002
    [7]
    赵珊珊, 高歌, 孙旭光, 等.西北太平洋热带气旋频数和强度变化趋势初探.应用气象学报, 2009, 20(5):555-563. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20090506&flag=1
    [8]
    高建芸, 江志红, 游立军, 等.百余年来影响福建热带气旋的变化特征.应用气象学报, 2007, 18(2):211-218. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20070236&flag=1
    [9]
    王东法, 陈海燕, 范爱芬, 等.浙江省热带气旋风雨空间分布特征研究.科技通报, 2010, 26(1):39-45. http://www.cnki.com.cn/Article/CJFDTOTAL-KJTB201001008.htm
    [10]
    孙莉莉, 陈爱莲, 王祥明, 等.山区台风灾害避灾行为的影响因素分析.自然灾害学报, 2010, 19(6):165-170. http://www.cnki.com.cn/Article/CJFDTOTAL-ZRZH201006024.htm
    [11]
    黄崇福, 刘安林, 王野.灾害风险基本定义的探讨.自然灾害学报, 2010, 19(6):8-16. http://www.cnki.com.cn/Article/CJFDTOTAL-ZRZH201006003.htm
    [12]
    扈海波, 王迎春, 刘伟东.气象灾害事件的数学形态学特征及空间表现.应用气象学报, 2007, 18(6):802-809. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=200706122&flag=1
    [13]
    黄沿波, 梁栋, 康雅乔, 等.风险的三维评价方法.自然灾害学报, 2010, 19(3):88-93. http://www.cnki.com.cn/Article/CJFDTOTAL-ZRZH201003015.htm
    [14]
    卞洁, 李双林, 何金海.长江中下游地区洪涝灾害风险性评估.应用气象学报, 2011, 22(5):604-611. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20110511&flag=1
    [15]
    李柏年.模糊数学及其应用.合肥:合肥工业出版社, 2007.
  • 加载中
  • -->

Catalog

    Figures(7)  / Tables(1)

    Article views (3212) PDF downloads(1199) Cited by()
    • Received : 2012-04-16
    • Accepted : 2012-09-19
    • Published : 2012-12-31

    /

    DownLoad:  Full-Size Img  PowerPoint