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Wang Xingzhi, Li Chongyin, Wang Guihua. A study on the surface current variation within half-year time scale in active region of the Kuroshio in East China Sea[J]. Haiyang Xuebao, 2014, 36(11): 1-11. doi: 10.3969/j.issn.0253-4193.2014.11.001
Citation: Wang Xingzhi, Li Chongyin, Wang Guihua. A study on the surface current variation within half-year time scale in active region of the Kuroshio in East China Sea[J]. Haiyang Xuebao, 2014, 36(11): 1-11. doi: 10.3969/j.issn.0253-4193.2014.11.001

A study on the surface current variation within half-year time scale in active region of the Kuroshio in East China Sea

doi: 10.3969/j.issn.0253-4193.2014.11.001
  • Received Date: 2013-10-23
  • Using high resolution data,the surface current variation within half-year time scale in active region of the Kuroshio in East China Sea is studied in this paper. The major results are as follows: (1) The northeast Taiwan area and near Tokara Strait region are two regions with the most remarkable variation of the surface current of Kuroshio in East China Sea (ECS). (2) There are the surface current variations within half-year time scale in two regions,the quasi-periodic transformation between anomalous cyclonic vortex and anomalous anticyclonic vortex is basic feature of the surface current variation. The spectrum peaks of the quasi-periodic transformation are mainly at 50 to 70 days and 90 to 140 days.(3)The actions of anomalous cyclonic vortex and anomalous anticyclonic vortex are closely related to the current axle variations of the Kuroshio in East China Sea,the action of anomalous cyclonic vortex (anticyclonic vortex) is accompanied with the flinching to southeast (the pushing on northwestwards) of the Kuroshio current axle. (4) In northeast of Taiwan area,the 50 to 70 days oscillation of the Kuroshio in East China Sea is mainly originated from the Kuroshio mesoscale fluctuation; the 90 to 140 days oscillation is mainly influenced by the mesoscale eddies from east of Taiwan. Analogously,the 50 to 70 days oscillation of the Kuroshio in East China Sea is mainly originated from the Kuroshio mesoscale fluctuation at upper reaches of the Kuroshio; the 90 to 140 days oscillation is mainly influenced by the mesoscale eddies from east of the Pyukyu gunto.
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  • 苏纪兰,刘先炳. 海洋环流研讨会论文选集[G]. 北京:海洋出版社,1992: 206-215.
    刘秦玉,刘倬腾,郑世培,等. 黑潮在吕宋海峡的形变及动力机制[J].青岛海洋大学学报,1996,26(4):413-420.
    袁耀初,苏纪兰. 1995年以来我国对黑潮及琉球海流的研究[J]. 科学通报,2000,45(22):2353-2356.
    Ichikawa K. Variation of the Kuroshio in the Tokara Strait induced by mesoscale eddies[J]. J Oceanogr,2001,57: 55-68.
    贾英来,刘秦玉,刘伟,等. 台湾以东黑潮流量的年际变化特征[J]. 海洋与湖沼,2004,35(6):507-512
    Nakamura,H. Numerical study on the Kuroshio path states in the northern Okinawa Trough of the East China Sea[J]. J Geophys Res,2005,110: C04003.
    袁耀初,杨成浩,王彰贵. 2000年东海黑潮和琉球群岛以东海流的变异Ⅰ.东海黑潮及其附近中尺度涡的变异[J]. 海洋通报,2006,28(2):1-13.
    管秉贤,袁耀初. 中国近海及其附近海域若干涡旋研究综述 Ⅰ.南海和台湾以东海域[J]. 海洋学报,2006,28(3):1-16.
    胡筱敏,熊学军,乔方利,等. 利用漂流浮标资料对黑潮及其邻近海域表层流场及其季节分布特征的分析研究[J]. 海洋学报,2008,30(6):1-16.
    李崇银,龙振夏. 冬季黑潮增暖对我国东部汛期降水影响的数值模拟研究[M]//气候变化若干问题研究. 北京:科学出版社,1992: 145-156.
    叶笃正,黄荣辉. 长江黄河流域旱涝规律和成因研究[M]. 济南:山东科学技术出版社,1996.
    Xu H,Xu M,Xie S P,et al. Deep atmospheric response to the spring Kuroshio Current over the East China Sea[J]. J Climate,2011,24: 4959-4972.
    蔡榕硕,陈际龙,谭红建.全球变暖背景下中国近海表层海温变异及其与东亚季风的关系[J].气候与环境研究,2011,16(1): 94-104.
    Yang Y,Liu C T,Hu J H. Taiwan Current (Kuroshio) and impinging eddies[J]. J Oceanogr,1999,55: 609-617.
    Zhang D,Johns W E,Lee T N,et al. The Kuroshio east of Taiwan: Modes of variability and relationship to interior mesoscale eddies[J]. J Phys Oceangr,2001(31): 1054-1074.
    Liu W,Liu Q,Jia Y. The Kuroshio Transport East of Taiwan and the Sea Surface Height Anomaly from the Interior Ocean[J]. Journal of Ocean University of China,2004,3: 135-140.
    刘伟. 斜压Rossby波与台湾以东黑潮[D]. 青岛:中国海洋大学,2005.
    林霄沛. 副热带海区季节内Rossby长波及其对东海黑潮的影响[D]. 青岛:中国海洋大学,2004.
    金宝刚. 北太平洋西边界流-中尺度涡相互作用研究[D]. 南京:解放军理工大学,2011.
    Wu C R,Lu H F,Chao S Y. A numerical study on the formation of upwelling off northeast Taiwan[J]. J Geophys Res,2008,113: C08025.
    朱小华. 琉球海流的研究进展[J]. 海洋学报,2008,30(5):1-8.
    郑小童,刘秦玉,胡海波,等. 琉球群岛以东的西边界流与东海黑潮流量时空特征的研究[J]. 海洋学报,2008,30(1):1-9.
    Johns W E,Lee T N,Zhang D,et al. The Kuroshio east of Taiwan: Moored transport observations from the WOCE PCM-1 array[J]. J Phys Oceaogr,2001,32: 1031-1053.
    靖春生,李立朱,大勇. 西太平洋-南海中尺度水位波动的耦合传播特征[J]. 科学通报,2006,51(20):2422-2428.
    Andres M,Park J H,Wimbush M,et al. Manifestation of the Pacific Decadal Oscillation in the Kuroshio[J]. Geophys Res Lett,2009,36: L16602.
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