数值实验论证台湾暖流和对马暖流的关系

郑沛楠; 白志鹏; 吴德星; 林霄沛

数值实验论证台湾暖流和对马暖流的关系

1.
中国海洋大学, 物理海洋实验室, 山东, 青岛, 266100;解放军61741部队, 北京, 100081
2.
解放军61741部队, 北京, 100081
3.
中国海洋大学, 物理海洋实验室, 山东, 青岛, 266100

基金项目: 国家基础研究规划项目(2005CB422302,2007CB411804);国家自然科学基金项目(40706006);教育部新世纪优秀人才计划(NECT-07-0781);高等学校引智计划(B07036);国际合作计划(2006DFB21250)

计量
- 文章访问数: 814
- HTML全文浏览量: 17
- PDF下载量: 1265
- 被引次数: 0
出版历程
- 收稿日期: 2008-08-05
- 修回日期: 2008-12-13

The remote connection of the Taiwan and Tsushima warm currents

1.
Physical Oceanography Laboratory, Ocean University of China, Qingdao 266100, China;The 61741 Army of the PLA, Beijing 100081, China
2.
The 61741 Army of the PLA, Beijing 100081, China
3.
Physical Oceanography Laboratory, Ocean University of China, Qingdao 266100, China

摘要

摘要: 台湾暖流和对马暖流均为沿中国东部海域大陆架的北向流。有学者认为存在"台湾-对马暖流流系"。现有的研究均未涉及台湾暖流和对马暖流在该系统中各自的动力作用。本文作者发现在该系统中对马暖流扮演更为重要的角色。借助一个三维斜压模式,作者设计了几组数值实验来讨论台湾暖流和对马暖流之间的动力学机制。结果显示台湾暖流对对马暖流几乎没有影响,而对马暖流却对台湾暖流存在重要影响。尽管对马暖流位于"下游区",通过"源-汇"驱动作用,其可以诱生约0.5×10⁶m³/s的台湾暖流水。作者认为,能量通过地形波传导理论可能为这一动力学机制的合理解释。
- 台湾-对马暖流系统 /
- POM /
- 源-汇驱动环流 /
- 地形波传导
Abstract: The Taiwan Warm Current(TWC)and the Tsushima Warm Current(TSWC)flow northward over the shelf in the East China Sea(ECS).Some previous studies consider them as a Taiwan-Tsushima Warm Current(TTWC)System.It seems that the TWC is dominant in the TTWC system because it is located at the "upst ream" region of the whole system.In this paper,however,we find that the TSWC is more important in the TTWC system.Using a three-dimensional baroclinic model,we conduct several experiments to discuss the dynamic relationship between the TWC and TSWC.The results show that the TWC has little effect on the TSWC,while the TSWC has a significant effect on the TWC.We use source-sink driven mechanism along isobaths to explain this phenomenon.The perennial northward flow through the Tsushima Strait pumps the response over the northern shelf in the ECS that gives rise to the TWC.Although the TSWCis located at the "downstream" region,it could induce 0.5 Sv to TWC in annual mean. The possible mechanism can be explained here in terms of energy propagation by topographic waves.
- Taiwan-Tsushima warm current system /
- POM /
- source-sink driven circulation /

HTML全文

参考文献(21)

YANG J,WU D,LIN X The Kuroshio forcing of the subtropical East Asian Marginal Seas[J].Journal of Physical Oceanography,2009,in press.

林葵,汤毓祥,郭炳火.黄海、东海表、上层实测流分析[J].海洋学报,2002,24(2):9-19.

FANG G,ZHAO B,ZHU Y.Water volume translport through the Taiwan Strait and the continental shelf of the East China Sea meas-ured with current meters[C]//Takara K.Oceanography of Asian Marginal seas.New York:Elsevier,1991:345-358.

SU J,PAN Y,LIANG X.Kuroshio intrusion and Taiwan Warm Current[G]//Oceanology of China seas.Netherlands:Kluwer Aca-demic Publishers,1994,1:59-70.

ZHU J,CHEN C,DING P,et al.Does the Taiwan warm current exist in winter?[J].Geophysical Research Letters,2004,31,L12302.doi.10.1029.

TEAGUE W J,JACOBS G A,KO D S,et al.Connectivity of the Taiwan,Cheju,and Korea Strait[J].Continental shelf Research,2003,23:63-77.

郭炳火,汤毓祥,葛人峰,等.台湾暖流和入侵陆架黑潮水的季节变化[J].海洋学报,2000,22(增刊):23-38.

ISOBE A On the origin of the Tsushima Warm Current and its seasonality[J].Continental Shelf Research,1999,19:117-133.

TAKIKAWA T,YOON J-H,CHO K-D.The Tsushima Warm Current through Tshushim Straits estimated from ferryboat ADCP[J].Journal of Physical Oceanography,2005,35:1154-1168.

ISOBE A.The Taiwan-Tsushima Warm Current system.Its path and the transformatjon of the water mass in the East China Sea[J].Journal of Oceanography,1999,55:185-195.

KIM K R,CHO Y K,KANG D J,et al.The Orign of the Tsushima Current based on oxygen isotope measurement[J].Geophysical Research Letter,2004,32,L03602,doi.10.1029.

GUAN B,FANG G.Winter counter-wind currents off the southeastern China coast:A review[J].Journal of Oceanography,2006,62:1-24.

GEORGE L Mellor.Users Guide for A Three-Dimensional,Primitive Equation,Numerical Ocean Model Program in Atmospheric and Oceanic Sciences[M].Princeton:Princeton University,NJ 08544-0710,2004.

Digital Relief of the Surface of the Earth.NOAA.National Geophysical Data Center,Boulder,Colorado,Data Announcement 93-MGG-01,1993.

Da SILVA A M,YOUNG C C,LEVITUS S.Atlas of Sudace Marine Data 1994,Volume 3,Anomalies of Heat and Momentum Flu-xes.NOAA Atlas NESDIS 8,U.s.Department of Commerce,NOAA,NESDIS,1994:411.

WORLEY S J,WOODRUFF S D,REYNOLDS R W,et al.ICOADS Release 2.1 data and products[J].International Journal of Cli-matology(CLIMAR-II Special Issue),2005,25:823-842.

KISTLER R,KALNAY E,COLLINS W,et al.The NCEP-NCAR 50-Year Reanalysis[R]//Monthly Means CD-ROM and Documenta-tion Bull Amer Meteor Soc,2001,82:247-268.

XIA Ch,QIAO F,ZHANG Q,et al.Numerical modeling of the Quasi-global Ocean circulation based on POM[J].Journal of Hydrody-namics.Ser.B,2004,16(5):537-543.

HU D,BAI X,PANG Ch.Seasonal variations of circulation and suspended matter transport in the yellow and east China seas[J].Jour-nal of Hydrodynamics,Ser.B,2001,4:8-13.

WANG F,HU D,BAI H,et al.Cyclonic recireulation on the left side of the Kuroshio in the East China Sea[J].Journal of Hydrody-namics,Ser.B,2001,3:133-137.

FANG G,ZHAO B.A note On the main forcing of the northeastward flowing current off the southeast China coast[J].Progress in O-ceanography,1988:21(3):363-372.

施引文献

资源附件(0)

访问统计