琉球海流的研究进展

朱小华

琉球海流的研究进展

朱小华

国家海洋局第二海洋研究所, 卫星海洋环境动力学国家重点实验室, 浙江, 杭州, 310012

基金项目: 国家自然科学基金项目(40776021);国家重点基础研究发展规划项目(2006CB400603);浙江省钱江人才计划(2007R10035)

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出版历程
- 收稿日期: 2008-01-10
- 修回日期: 2008-06-24

Overview of studies on the Ryukyu Current

ZHU Xiao-hua

State Key Laboratory of Satellite Ocean Environment Dynamics Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China

摘要

摘要: 文章对近期有关琉球海流的研究进行了综述。指出琉球海流是北太平洋一支重要的西边界流,具有如下特征:琉球海流的表层部分受中尺度涡影响强烈,其流速和流量存在有较稳定的次表层极大值,琉球海流在冲绳岛和奄美大岛间得到了显著增强,是一支可和黑潮相匹敌的海流。有关琉球海流的以下几方面内容有待今后更深入研究:(1)琉球海流的起源,其形成的动力学机制及琉球海流在冲绳岛以南的时空变化;(2)琉球海流次表层极大值形成、维持及在冲绳岛以北得到显著增强的动力学机制;(3)琉球海流对东海的影响及其水和热流量在黑潮中所起的作用。
- 琉球海流 /
- 黑潮 /
- 次表层流核 /
- 流速和流量 /
- 动力学机制
Abstract: The recent study achievementaboutthe Ryukyu Current(RC)is reviewed.It is pointed outthat the RC is animportant western boundary current in the North Pacific.The RC is strongly influenced by the mesoscale eddy and its velocity and volume transportex hibits subsurface maximum structure.The RC remarkably develops between the Okinawa and Amami-Ohshima Islands.The following three points need to betteraddress:(1)the origin of the RC,the formation mechanism and its temporal and spatial variations;(2)dynamic processes offormation and maintaining of the subsurface maximum structure,the development of RC from the northern of the Okinawa Island,and(3)the contributions of volume and heat transport to the Kuroshio.
- the Ryukyu Current /
- the Kuroshio /
- subsurface maximum structure /
- velocity and volume transport /
- dynamic processes

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参考文献(39)

NITANI H.Beginning of the Kuroshio[M].STOMMEL H,YOSHIDA K.Kuroshio:Its Physical Aspects.Tokyo:Univ Tokyo Press,1972z129-163.

WANG Yuan-pei,SUN Xiao-ping.A study on the features of Ryukyu Current[C].Proceedings of investigation of Kuroshio,No.2.Beijing:China Ocean Press,1990:237-245.

YUAN Yao-chu,TAKANO K,PAN Zi-qin,et al.The Kuroshio east in the East China Sea and the currents east of Ryukyu Islands during autumn 1991[J].Lamer,1994,32:235-224.

YUAN Yao-chu,SU Ji-lan,PAN Zi-qin,et al.The west boundary current east of Ryukyu Islands[J].La met,1995,33:1-11.

YU Hong-hua,SU Ji-lan,MIAO Yu-tian.Low Salinity Water (LSW) core of Kuroshio in the East China Sea and intrusion of Western Boundary Current (WBC) East of Ryukyu Islands[C].Proceedings of China-Japan Joint Symposium of the Cooperative Research on the Kuroshio,Qingdao,China,27-29 October 1992.Beijing:China Ocean Press,1994:145-163.

SU Ji-lian.Circulation dynamics of the China seas north of 18～N[M]//ALLAN R R,KENNETH H B.The Sea,Vol.11.John Wiley Sons,Inc,1998..483-505.

袁耀初,苏纪兰.1995年以来我国对黑潮及琉球海流的研究口].科学通报,2000,45(22):2353-2356.

胡珀,侯一筠,乐肯堂,等.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.

IMAWAKI S,UCHIDA H,ICHIKAWA H,et al.Satellite altimeter monitoring the Kuroshio transport south of Japan[J].Geophys Res Lett,2001,28:17-20.

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 Oceanogr,2001,31:1031-1053.

ICHIKAWA H,BEARDSLEY R C.Temporal and spatial variability of volume transport of the Kuroshio in the East Chian Sea[J].Deep-Sea Res,1993,40:583-605.

ANDRES M,WIMBUSH M,PARK J-H,et al.Observations of Kuroshio flow variations in the East China Sea[J/OL].J Geophys Res,2008,Vol.113,C05013,doi: 10.1029/2007JC004200.

NAKANO T,KURAGANO T,LIU Y.Variations of oceanic conditions east of the Ryukyu Islands[C].Proceedings of Japan and China Joint Symposium on Cooperative Study of Subtropical Circulation System,1-4 December 1997.Nagasaki:Nagasaki Japan,Seikai National Fisheries Research Institute,Nagasaki,1998:129-140.

YANG Y,LIU C-T,HU J-H,et al.Taiwan Current (Kuroshio) and impinging eddies[J].J Oceanogr,1999,55:609-617.

ZHU Xiao-Hua,ICHIKAWA H,ICHIKAWA K,et al.Variability of the volume transport southeast of Okinawa Island estimated from satellite altimeter data[J].J Oeeanogr,2004,60:953-962.

YUAN Yao-chu,SU Ji-lan,PAN Zi-qin et al.The west boundary current east of Ryukyu Islands[J].Lamer,1995,33:1-11.

SHIGA T,UENO D,TAKATSUKI Y,et al.Variations of oceanic conditions east of the Ryukyu Islands in 1997[C].Proceedings of Japan and China Joint Symposium on Cooperative Study of Subtropical Circulation System.Beijing:China Ocean Press,2000:57-65.

ICHIKAWA H,NAKAMURA H,NISHINA A,et al.Variability of northeastward current southeast of northern Ryukyu Islands[J].J Oeeanogr,2004,60:351-363.

朱小华、黄大吉.2004-2006年奄美大岛以东的琉球海流[J].地球物理学报,2008,51(5):1354-1363.

ZHU Xiao-Hua,HAN I-S,PARK J-H,et al.The northeastward current southeast of Okinawa Island observed during November 2000 to August 2001[J/OL1.Geophys Res Lett,2003,30:1071,doi: 10.1029/2002GL015867.

ZHU Xiao-Hua,PARK J-H,KANEKO I.The northeastward current southeast of Ryukyu Islands in early winter of 2000 estimated by an inverse technique[J/OL].Geophys Res Lett,2005,32:L05608,doi: 10.1029/2004GL022135.

ZHU Xiao-Hua,PARK J-H,KANEKO I.Velocity structures and transports of the Kuroshio and the Ryukyu Current during fall of 2000 estimated by an inverse technique[J].J Oeeanogr,2006,62:587-596.

ZHU Xiao-Hua,KANEKO A,SAITO T,et al.Kuroshio stream path variation and its associated velocity structures south of Shikoku,Japan[J].Geophys Res Lett,2001,28:4615-4618.

ANDRES M,PARK J-H,WIMBUSH M,et al.Study of the Kuroshio/Ryukyu Current system based on satellite-altimeter and in situ measurements[J].(submitted to J.Oceanogr.).

NAGANO A,ICHIKAWA H,MIURA T,et al.Current system east of the Ryukyu Islands[J/OL].J Geophys Res,2007,112,C06009,doi: 10.1029/2006JC0003917.

ZHU Xiao-Hua,PARK J-H,WIMBUSH M,et al.Comment on "Current system east of the Ryukyu Islands" by A.Nagano et al.[J/OL].Journal of Geophysical Research,2008,113,C03020,doi: 10.1029/2007JC004458

NAGANO A.,ICHIKAWA H,MIURA T,et al.Reply to comment by Xiao-Hua et al.on "Current system east of the Ryukyu Islands"[J/OL].J Geophys Res,2007,113,C03021,doi: 10.1029/2007JC0004561.

ZHU Xiao-Hua,PARK J-H,WIMBUSH M,et al.The Ryukyu Current during October 2002-Reanalysis of the Cruise Data-[C].Expanded Abstract of 2008 Japan Oceanographic,Society Spring meeting,2008:125.

袁耀初,管秉贤.中国近海及其附近海域若干涡旋研究综述:Ⅱ.东海和琉球群岛以东海域[J].海洋学报.2007,29(2):1-17.

QIU B.Seasonal eddy field modulation of the North Pacific Subtropical Countercurrent:TOPEX/Poseidon observations and theory[J].J Phys Oceanogr,1999,29:2471-2486.

TAKIGAWA T,ICHIKAWA H,ICHIKAWA K,et al.Extraordinary subsurface mesoscale eddy detected in the southeast ot Okinawa in February 2002[J/OL].Geophys Res Lett,2005,32:L17602,doi: 10.1029/2005GL023842.

EBUCHI N,HANAWA K.Trajectory of mesoscale eddies in the Kuroshio recirculation region[J].J Oceanogr,2001,60:351-363.

ICHIKAWA K.Variation of the Kurohsio in the Tokara Strait induced by meso-scale eddies[J].J Oceanogr,2001,57:55-68.

ZHU Xiao-Hua,PARK J-H,HUANG Da-ji.Observation of baroclinic eddies southeast of Okiniawa Island[J/OL].Science in China Series-D,2008,doi:10.1007/s 1430-008-0146-9.

YUAN Yao-chu,KANEKO A,SU Ji-lan,et al.The Kuroshio east of Taiwan and in the East China Sea and the currents east of Ryukyu Islands during early summer of 1996[J].J Oceanogr,1998,54:217-226.

LEE T N,JOHNS W E,LIU C-T,et al.Mean transport and seasonal cycle of the Kurhoshio east Taiwan with comparison to the Florida Current[J].J Geophys Res,2001,106(C10):22143-22158.

SEKINE Y,KUTSUWADA K.Seasonal variation in volume transport of the Kuroshio south of Japan[J].J Phys Oceanogr,1994,24:261-272.

YOU S-H,YOON J-H.Modeling of the Ryukyu Current along the Pacific side ofo the Ryukyu Islands[J].Phys Oceanogr,2004(2):44-51.

NAKAMURA H,ICHIKAWA H,NISHINA A.Numerical study of the dynamics of the Ryukyu Current system[J/OL].J Geophys Res,2007,112,C04016,doi: 10.1029/2006JC003595.

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