首页期刊介绍通知公告编 委 会投稿须知电子期刊广告合作联系我们在线留言
 
北部湾台风风暴潮数值模拟及重点区域风险分析
作者:蒋昌波1 2  赵兵兵1  邓斌1 2  伍志元1 
单位:1. 长沙理工大学 水利工程学院, 湖南 长沙 410004;
2. 水科学与水灾害防治湖南省重点实验室, 湖南 长沙 410004
关键词:Delft3D 风暴潮 蒙特卡罗 风险分析 
分类号:P731.23
出版年·卷·期(页码):2017·34·第三期(32-40)
摘要:
基于Delft3D模型建立了适用于北部湾海域的台风风暴潮数学模型,同时根据进入北部湾海域67 a (1949—2015年)历史台风资料,采用蒙特卡罗方法随机构造55场台风进行风暴增水计算,并选取受风暴潮影响最严重的铁山港与最频繁的涠洲岛进行了风险分析。结果表明:(1)从铁山湾下侧进入北部湾海域,中心气压为952 hPa的台风会造成石头埠站风暴增水为3.68 m,达到1 000 a一遇的级别;(2)广西沿岸的风暴增水对经过北部湾海域的台风存在滞后效应;(3)涠洲岛风暴增水普遍较低,但进入北部湾的台风均会在涠洲岛产生风暴潮,因此要做好涠洲岛的防护工程以防止海岸线继续后退。
A mathematic model of typhoon storm surge for the Beibu Gulf was established based on Delft3D hydrodynamic models,and the Monte Carlo method was used to generate 55 typhoons randomly according to the historical typhoon data of 67 a (1949—2015) in the Beibu Gulf.A study on hazard research of the most severe area (Tieshan Bay) and the most frequent area (Weizhou Island) affected by storm surge has been carried out by storm surge calculation with the generated typhoons.The result showed that (1) the surge at Shitoubu station affected by a typhoon with central pressure of 952 hPa is 3.68 m which return period is 1 000 a.(2) The storm surge at the coast of Guangxi has lagged effect on the typhoon passing through the Beibu Gulf.(3) The storm surge at Weizhou Island is generally low,but the typhoon into the Beibu Gulf will generate a storm surge here.Hence,the protection project at Weizhou Island should be prepared to prevent the coastline continues to retreat.
参考文献:
[1] 陈宪云,刘晖,董德信,等.广西主要海洋灾害风险分析[J].广西科学,2013,20(3):248-253.
[2] Irish J L,Resio D T,Ratcliff J J.The influence of storm size on hurricane surge[J].Journal of Physical Oceanography,2008,38(9):2003-2013.
[3] Lima R J,Li C Y.On the importance of the forward speed of hurricanes in storm surge forecasting:A numerical study[J].Geophysical Research Letters,2009,36(7):L07609.
[4] Xie L,Wu K J,Pietrafesa L,et al.A numerical study of wave-current interaction through surface and bottom stresses:Wind-driven circulation in the South Atlantic Bight under uniform winds[J].Journal of Geophysical Research:Oceans,2001,106(C8):16841-16855.
[5] 冯士筰.风暴潮导论[M].北京:科学出版社,1982.
[6] 李树华,陈文广,陈波,等.广西沿海台风暴潮数值模拟试验[J].海洋学报,1992,14(5):15-25.
[7] 李树华.珍珠港台风暴潮特征及其预报的初步研究[J].海洋预报,1986,3(4):17-24.
[8] 陈波,魏更生.广西沿海风暴潮的数值计算研究[J].海洋湖沼通报,2002(1):1-8.
[9] 陈波,邱绍芳.广西沿海港湾风暴潮增减水与台风路径和地形效应的关系[J].广西科学,2000,7(4):282-285.
[10] Gomes M P,Pinho J L,Do Carmo J S A,et al.Hazard assessment of storm events for The Battery,New York[J].Ocean&Coastal Management,2015,118:22-31.
[11] 黄潘阳,叶银灿,韦雁机,等."威马逊"台风暴潮增水及水动力响应数值模拟[J].海洋预报,2012,29(2):32-38.
[12] Deltares.Wind Enhanced Scheme (WES) for Cyclone Modelling[M].2014.
[13] 刘永玲,冯建龙,江文胜,等.热带气旋资料长度对风暴潮危险性评估结果的影响[J].海洋学报,2016,38(3):60-70.
[14] 纪燕新.北部湾广西沿海风暴潮灾害及防灾减灾研究[D].南宁:广西大学,2007.
[15] 中国国际标准化管理委员会.GB/T 19201-2006热带气旋等级[S].北京:中国标准出版社,2006.
[16] 李明杰,吴少华,刘秋兴,等.风暴潮、大潮对广西涠洲岛西南沙滩侵蚀的影响分析[J].海洋学报,2015,37(9):126-137.
[17] 姚子恒,高伟,高珊,等.广西北海涠洲岛海岸侵蚀特征[J].海岸工程,2013,32(4):31-40.
服务与反馈:
文章下载】【发表评论】【查看评论】【加入收藏
 
 海洋预报编辑部 地址:北京海淀大慧寺路8号
电话:010-62105776
投稿网址:http://www.hyyb.org.cn
邮箱:bjb@nmefc.cn