OALib Journal期刊
ISSN: 2333-9721
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钦州湾台风浪的多年一遇极值推算
Keywords: 钦州湾,海浪模式,皮尔逊ⅲ(p-ⅲ)频率适线法,多年一遇
Abstract:
?利用wavewatchⅲ(ww3)和swan海浪模式模拟了1949—2005年间对钦州湾海域影响较大的台风浪。以模拟结果为基础,利用皮尔逊ⅲ(p-ⅲ)频率适线法推算了钦州湾湾外深水的累积频率波高和平均波周期(tm)的多年一遇极值,同时模拟了其间在百年一遇高潮水位条件下的台风浪,以及在百年一遇高潮水位、百年一遇风暴潮增水共同作用下对钦州湾影响较大的台风产生的波浪场。使用p-ⅲ法推算了在极端天气下,钦州湾湾内统计点的累积波高和平均波周期的多年一遇极值。研究结果表明,由于湾内浅滩较多,波浪在传播过程中水体底部摩擦使能量耗损明显,所以湾内波高较小,湾口处的波高大于内湾处的波高。近岸海区的波浪耗散、破碎等物理过程比较强烈,因此近岸统计点c1处的波高极值最小,其最大波高向岸边快速减弱并沿东向传播。在极端天气情况下,波浪在传播过程中发生破碎,波高衰减显著。
References
[1] | 刘月红.钦州湾波浪条件数值模拟研究[j].港工技术,2007,10(5):8-16.冯芒,沙文钰,朱首贤.近岸海浪几种数值计算模型的比较[j].海洋预报,2003,20(1):52-59.李树华,夏华永,陈明剑.广西近海水文及水位动力环境研究[m].北京:海洋出版社,2001:67-71.tolmanhl,balasubramaniyanb,burroughsld,etal.developmentandimplementationofwindgeneratedoceansurfacewavemodelsatncep[j].weatherandforecasting,2002,17(2):311-333.tolmanhl.usermanualandsystemdocumentationofwacewatchⅲversion2.22[r].washington,usa:noaa/nws/ncep,2002:1-139.tolmanhl.validationofanewglobalwaveforecastsystematncep[m].washington,usa:americansocietyofcivilengineers,1998:777-786.wingeartkm,reillywc,herbersthc,etal.validationofoperationalglobalwavepredictionmodelswithspectralbuoydata[m].washington,usa:americansocietyofcivilengineers,2001:590-599.risrc,holthuijsenlh,booijn.athird-generationwavemodelforcoastalregions2.verfication[j].journalofgeophysicalresearch,1999,104(c4):7667-7681.rogerswe,kaihatu,jm,hsul,etal.forecastingandhindcastingwaveswiththeswanmodelinthesoutherncaliforniabight[j].coastalengineering,2007,54:1-15.tolmanhl.thenumericalmodelwavewatch:athirdgenerationmodelforthehindcastingofwindwavesontidesinshelfseas[r]//communicationonhydraulicandgeotechnicalengineering.delhi:delhiuniversityoftechnology.,1989,reportno.89-2.holthuijsenlh,tolmanhl.effectsofthegulfstreamonoceanwaves[j].journalofgeophysical.research,1991,96(c7):12755–12771.tolmanhl.effectsofnumericsonthephysicsinathird-generationwind-wavemodel[j].journalofphysicaloceanography,1992,22:1095-1111.booijn,holthuijsenlh,risrc.theswanwavemodelforshallowwater[c]//proceedingof24thinternationalconferenceoncoastalengineering.orlando,1996:668-676.booijn,risrc,holthuusenlh.athird-generationwavemodelforcoastalregion.partⅰ:modeldescriptionandvalidation[j].j.geophys.res,1999,104(c4):7649-7666.张志旭,齐义泉,施平,等.波致应力对台风天气下南海上层海流的影响分析[j].热带海洋学报,2007,26(1):1-8.文圣长,余宙文.海浪理论与计算原理[m].北京:科学出版社,1985:127-141.高山,丁平兴,朱首贤.wavewatch的操作系统移植及其与swan嵌套接口的改进[j].海洋科学进展,2006,24(2):228-237.kalnaye,kanamitsum,kustkerr,etal.thencep/ncar40-yearreannalisisproject[j].bullammeteorolsoc,1996,77(3):437-471.joseysa,kentec,taylorpk.windstressforcingoftheoceaninthesocclimatology:comparisonswiththencep-ncar,ecmwf,uwm/coads,andhellermanandrosensteindatasets[j].journalofphysicaloceanography,2002,32:1993-2019.hollandgj.ananalyticmodelofthewindandpressureprofilesinhurricanes[j].monwearev,1980,108:421-427.么枕生.气候统计[m].北京:气象出版社,1991:124-131.史勇军,吴忠良,白玲.用皮尔逊检验分析年度地震趋势预测结果[j].中国科学院研究生院学报,2004,21(2):248-253.交通部第一航务工程勘察设计院.海港水文规范[s].北京:人民交通出版社,2004:4-50.董胜,孔令双.海洋工程环境概论[m].青岛:中国海洋大学出版社,2005:43-49.韩树宗,王海龙,郭佩芳.利用卫星高度计资料进行多年一遇极值波高的方法研究[j].青岛海洋大学学报,2003,33(5):657-664panj.discussiononlongseriesdistributionofyearlymaximumwaves[j].oceanengineering,1983,2(1):9-37.潘锦娥.年极值重现期波高的探讨[j].海洋工程,1983,(2):29-37.huj,jiangh.theresearchonforecastingclimateextremevaluebygumbellmethod[j].journalofoceanuniversityofqingdao,1993,23(1):43-51.宋运法,尹毅,王昭正.广西防城港核电报告[r].广州:中国科学院南海海洋研究所,2010:1-378.
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