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1991-2011年东海黑潮PN断面流结构与季节变化分析 被引量:2

Analysis of current structure and seasonal variation at PN Section of the East China Sea Kuroshio during 1991-2011
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摘要 基于日本海洋信息中心提供的东海黑潮PN断面CTD资料,本文采用动力高度法计算了1991-2011年间90个航次的断面流速,并对流场结构、最大流速、流幅和流量进行了统计分析。结果表明:东海黑潮PN断面流场存在单核、双核、多核3种结构;其中单核结构出现的概率为50%,双核结构为39%,多核结构为11%。东海黑潮的流结构存在显著的季节变化:秋季多核结构所占的比重为4个季节最大,平均流核数最多;冬季主要为单核结构,平均流核数最少;夏季和春季则没有明显的倾向性,单核、双核、多核3种结构出现概率相近,平均流核数介于秋季和冬季之间。其次东海黑潮的流量也存在显著的季节变化:冬季与夏季最强,秋季最小,春季居中。最后东海黑潮的最大流速和流幅也存在季节变化:夏季最大,秋季最小,春季和冬季居中。 Based on the CTD data of PN Section provided by Japanese Oceanographic Data Center,the current velocity of ninety cruises during 1991 to 2011are calculated with dynamic height method.The structure,maximum velocity,flux and width of the current are analyzed.The results show that there are three kinds of typical current structure of Kuroshio at PN Section,which are single core structure,double-core structure and multi-core structure.The occurrence probability of single core,double-core and multi-core are 50%,39%and 11%respectively.The current structure of Kuroshio at PN section exhibits significant seasonal variation.In autumn,the probability of occurrence of multi-core structure reaches its maximum,and the quarterly average of current core number is greater than other seasons.In winter,multi-core structure never emerges and single core structure occurs more often than any other structures,and the quarterly average of current core number is less than other seasons.All kinds of current structure occur in spring and summer.The quarterly average of current core number of spring and summer are between autumn and winter.The flux of Kuroshio at PN Section exhibits seasonal variation too.The flux reaches the largest in winter and summer,and smallest in autumn.Seasonal variation also occurs in maximum velocity and current width of Kuroshio at PN Section,which are the largest in summer and the smallest in autumn,followed by spring and winter.
出处 《海洋学报》 CAS CSCD 北大核心 2016年第5期14-26,共13页
关键词 东海 黑潮 PN断面 流速结构 季节变化 East China Sea Kuroshio PN Section current structure seasonal variation
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  • 1管秉贤. 东海G断面上二十年(1956-1975)来黑潮表层流速的变动[J]. 科学通报, 1973(21): 990-994.
  • 2赤松英雄. 东シナ海この观测かぅ[J]. 海洋科学, 1979, 11(3): 175-181.
  • 3井上尚文. 东シナ海まょひ对马暖流域にすけゐ流况[G]. 长崎县生物学会文集, 1981: 29-72.
  • 4袁耀初, 远藤昌宏, 石崎广. 东海黑潮与琉球群岛以东海流的研究[G]//黑潮调查研究论文选(三). 北京: 海洋出版社, 1991: 220-234.
  • 5袁耀初, 潘子勤, 金子郁雄, 等. 东海黑潮的变异与琉球群岛以东海流[G]//黑潮调查研究论文选(五). 北京: 海洋出版社, 1993: 279-297.
  • 6孙湘平, 王元培, 袁启科, 等. 1986-1988年黑潮的路径、流速和流量[G]//黑潮调查研究论文集(三). 北京: 海洋出版社, 1991: 48-59.
  • 7孙湘平, 金子郁雄. 1989-1991黑潮的变异[G]//黑潮调查研究论文选(五). 北京: 海洋出版社, 1993: 52-68.
  • 8汤毓祥, 田代知二. 东海PN断面黑潮流况的分析[G]//黑潮调查论文集(五). 北京: 海洋出版社, 1993: 69-76.
  • 9陈红霞,袁业立,华锋.东海黑潮主段G-PN断面的多核结构[J].科学通报,2006,51(6):730-737. 被引量:13
  • 10汤毓祥,林葵,田代知二.关于东海黑潮流量某些特征的分析[J].海洋与湖沼,1994,25(6):643-651. 被引量:17

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