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机构地区:[1]Physical Oceanography Laboratory,Ocean University of China [2]Department of Marine,Earth,and Atmospheric Sciences,North Carolina State University
出 处:《Chinese Journal of Oceanology and Limnology》2014年第6期1435-1442,共8页中国海洋湖沼学报(英文版)
基 金:Supported by the Strategic Priority Research Program of Chinese Academy of Sciences(No.XDA11010103);the National Natural Science Foundation of China(Nos.41222037,41221063);the Project of Global Change and Air-Sea Interaction(No.GASI-03-01-01-02);the National Basic Research Program of China(973 Program)(No.2013CB956202);the 111 Project of Ministry of Education of China(No.B07036);the Natural Science Foundation of Shandong(No.JQ201111);the National Special Research Fund for Non-Profit Marine Sector(No.201205018)
摘 要:The self-organizing map method is applied to satellite-derived sea-level anomaly fields of1993-2012 to study variations of the Kuroshio intrusion northeast of Taiwan Island.Four major features are revealed,showing significant seasonal variability of the intrusion.In general,the intrusion increases(decreases) with a high(low) sea-level anomaly at the edge of the East China Sea shelf in winter(summer).Open-ocean mesoscale eddies play an additional role in modulating the seasonal variation of the intrusion.Further analyses are needed to study eddy-Kuroshio interaction dynamics.The self-organizing map method is applied to satellite-derived sea-level anomaly fields of 1993-2012 to study variations of the Kuroshio intrusion northeast of Taiwan Island. Four major features are revealed, showing significant seasonal variability of the intrusion. In general, the intrusion increases (decreases) with a high (low) sea-level anomaly at the edge of the East China Sea shelf in winter (summer). Open-ocean mesoscale eddies play an additional role in modulating the seasonal variation of the intrusion. Further analyses are needed to study eddy-Kuroshio interaction dynamics.
关 键 词:Kuroshio intrusion self-organizing map mesoscale eddies
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