| 东海黑潮及琉球群岛以东海流研究进展 |
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| 引用本文： | 胡珀,侯一筠,乐肯堂,王铮.东海黑潮及琉球群岛以东海流研究进展[J].海洋科学集刊,2007(48):28-34. |
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| 作者姓名： | 胡珀 侯一筠 乐肯堂 王铮 |
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| 作者单位： | 中国科学院海洋研究所，青岛266071
中国科学院研究生部，北京100039 |
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| 基金项目： | 国家重点自然科学基金“中国海黑潮区关键动力过程的非线性特征及其预测方法(90411013)” 和中国科学院创新方向项目(KZCX2-YW-201)资助 |
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| 摘 要： | 东海是西太平洋的一个边缘海,它西部有广阔的大陆架,东面以九州岛、琉球群岛(由奄美诸岛、冲绳诸岛、先岛诸岛组成)和台湾岛连线为界,具有较深的海槽。黑潮是一支高温、高盐、高流速的西边界流,它起源于菲律宾以东海域、流经台湾东岸进入东海,沿东海大陆架外缘向东北向流动，穿越吐噶喇海峡返回太平洋。通常的把自台湾东北端起至吐噶喇海峡一段称为东海黑潮。此外,在琉球群岛以东海域也常年存在一支稳定的西边界流,称为琉球海流。
对于东海黑潮和琉球海流的硏究,主要起步于20世纪80年代,通过进行中日联合调查研究、中日副热带环流调查研究等,取得了许多重要成果,苏纪兰(1994)、袁耀初(2000，Yuan,2006)、管秉贤(2002)等人都做过评述。本文基于以上研究评述,主要叙述200年以来对东海黑潮及琉球海流的硏究新进展。
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| 关 键 词： | 东海黑潮、琉球群岛、海流 |
| 收稿时间： | 2006/11/1 0:00:00 |
STUDY ADVANCES ON THE KUROSHIO IN THE EAST CHINA SEA AND CURRENTS IN THE REGION EAST OF RYUKYU ISLANDS |
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| Hu Po,Hou Yijun,Le Kentang,Wang Zheng.STUDY ADVANCES ON THE KUROSHIO IN THE EAST CHINA SEA AND CURRENTS IN THE REGION EAST OF RYUKYU ISLANDS[J].Studia Marina Sinica,2007(48):28-34. |
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| Authors: | Hu Po Hou Yijun Le Kentang Wang Zheng |
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| Institution: | Institute of Oceanology,Chinese Academy of Sciences, Qingdao 266071
Graduate School of Chinese Acadeny of Sciences, Beijing 100039;Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071 |
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| Abstract: | On the basis of study overview of SU Jilan, YUAN Yaochu and GUAN Bingxian,the recent study advances on the Kuroshio in the East China Sea(ESC)and currents in the region east of Ryukyu Islands are reviewed,especially since 2000 years. The most interested problems awaiting solution in the ESC are as follows;the structure variability of the Kuroshio main part, the Kuroshio intrusion northeast of Taiwan and southwest of Kyushu, meso-scale eddies on both sides of Kuroshio and so on. Study of east of Ryukyu Islands is concentrated on the Ryukyu Current,anti-cyclonic warm eddies and cyclonic cold eddies east of the Ryukyu Current. From the above analysis,finally, the author put forward some problems to be further studied. |
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