全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
-  2005 

渤海风驱-潮致拉格朗日余流的数值模拟与季相时空变异

DOI: 10.11821/yj2005030004

Keywords: 渤海,风驱-潮致拉格朗日余流,数值模拟,季相变化,时空变异

Full-Text   Cite this paper   Add to My Lib

Abstract:

摘要: 利用HellermanandRosenstein全球风应力资料中的多年月平均风场资料驱动ECOM模型,设计了潮致、纯风生以及风与潮两者叠加三个数值实验对渤海海域风驱-潮致拉格朗日(Lagrange)余流的逐月时空分布与季节变化进行了模拟。研究结果表明,季风的大小和方向决定了渤海风驱-潮致拉格朗日余流的大小和方向,是影响余流流向和流速的重要因素。冬季,从渤海西岸到莱州湾海域风驱-潮致拉格朗日余流表现出一个大逆时针环流,辽东湾呈现顺时针方向流动,渤海中部存在一个弱的顺时针流环。夏季,整个渤海海域呈现顺时针流况,渤海海盆存在一微弱的逆时针涡旋,一支西南向流沿辽东湾东岸穿越渤海海盆,与起自渤海湾的东向流一起进入莱州湾。风驱-潮致拉格朗日余流主要受风的控制,潮汐则起到一定的调整作用。

References

[1]  管秉贤.中国沿岸的表面海流与风的关系的初步研究.海洋与湖沼,1957,1(1):95~122.
[2]  郑连远.三维潮致拉格朗日余流的数值计算及其在渤海中的应用.青岛海洋大学学报,1992,22(1):39~49.
[3]  王辉.渤海三维风驱-热盐-潮致拉格朗日余流数值计算.海洋学报,1993,15(1):9~21.
[4]  Mao Hanli,Guan Bingxian. A note on t he circulation of t he East China Sea.Proceedings of t he J apan - China ocean st udy symposium on“Physical oceanograp hy and marine engineering in t he East China Sea”,October 28229,1981,special report of Instit ute of Oceanic Research,Shimizu:Tokai U niversit y,1~24.
[5]  窦振兴,张存智,张砚峰.渤海风海流数值计算.海洋学报,1986,8(5):527~533.
[6]  缪经榜,刘兴泉.北黄海和渤海冬季环流动力学数值实验.海洋学报,1989,11(1):15~22.
[7]  黄大吉,陈宗镛,苏纪兰.三维陆架海模式在渤海中的应用I.潮流、风驱环流及其相互作用.海洋学报,1996,18(5):1~15.
[8]  Feng Shizuo1 A t hree dimensional weakly nonlinear model of tide2induced Lagrangian residual current and masst ransport,wit h an application to t he Bohai Sea. In:Nihoul J C J,Jamart B M(eds1). Three Dimensional Modelsof Marine and Est uarine Dynamics. Elsevier Oceanography Publishers1 Amsterdam Oxford - New York,1987.471~488.
[9]  Feng Shizuo. On t he circulation in Bo hai Sea,Yellow Sea and East China Sea. In:Hong G H,et al.(eds.).Healt h of t he Yellow Sea. Korea:KORDI,19981 43~78.
[10]  魏皓.浅海环流物理的理论与数值研究.青岛:青岛海洋大学博士论文,1999.
[11]  Wei Hao,Wu Jianping1 Pohlmann Tho mas1 A simulation on t he seasonal variation of t he circulation and t ransportin t he Bohai Sea. Journal of Oceanography of Huanghai and Bohai Seas,2001,19(2),1~9.
[12]  Mellor G L,Yamada T1 Develop ment of a t urbulence clo sure model for geop hysical fluid p roblem1 Rev1 Geop hys.Space Phys.,1982,20:851~857.
[13]  顾玉荷,修日晨.渤海海流概况及其输沙作用初析.黄渤海海洋,1996,14(1):1~6.
[14]  王凯,冯士笮,施心慧.渤、黄、东海夏季环流的三维斜压模型.海洋与湖沼,2001,32(5):551~560.
[15]  管秉贤.有关我国近海海流研究的若干问题.海洋与湖沼,1962,4(3):121~141.
[16]  沈鸿书,毛汉礼.渤海及北黄海西部的基本水文特征.海洋科学集刊,1964,(增刊):1~10.
[17]  赵保仁,庄国文,曹德明.渤海的环流、潮余流及其对沉积物分布的影响.海洋与湖沼,1995,26(5):466~473.
[18]  Miao Jingbang,Liu Xingquan. A numerica. st udy of t he winter time circulation in t he Nort hern Huanghai Sea andt he Bo hai Sea,Part I:Basic characteristics of t he circulation1 Chinese Journal of Oceanology and Limnology,1988,(3):216~226.
[19]  Chio B. Note on current s driven by a steady uniform wind st ress on t he Yellow Sea and t he East China Sea,LaMer,1982,20:65~74.
[20]  张淑珍,奚盘根,冯世笮.渤海环流数值模拟.山东海洋学院学报,1984,14(2):12~18.
[21]  刘兴泉,缪经榜,季仲贞.渤海冬季环流数值研究.大气科学,1989,13(3):280~288.
[22]  Zhao Jinping,Shi Maochong. Numerical modeling of t he t hree2dimensional characteristics of t he wind driven current in t he Bohai Sea1 Chinese Journal of Oceonology and Limnology,1993,11(1):70~79.
[23]  赵保仁,曹德明.渤海冬季环流形成机制动力学分析及数值研究1海洋与湖沼,1998,29(1):86~96.
[24]  Feng Shizuo1 A t hree-dimensional weakly nonlinear dynamics on tide-induced Lagrangian residual current and masst ransport1 Chinese Journal of Oceanology and Limnology,1986,4(2):129~158.
[25]  Feng Shizuo,Cheng Ralp h T,Xi Pangen. On tide-induced Lagrangian residual current and residual t ransport1 Water Resources Research,1986,22(12):1623~1646.
[26]  黄祖珂,王学昌. ADI法的计算结果及分析.山东海洋学院学报,1988,18(2):48~49.
[27]  王化桐.有限元法的计算结果及分析.山东海洋学院学报,1988,18(2):49~50.
[28]  Sun Wenxin,Xi Pangen,Song Lina1 Numerical calculation of t he t hree2dimensional tide2induced Lagrangian residual circulation in t he Bo hai Sea. Journal of Ocean University of Qingdao,1989,19(2):27~36.
[29]  王辉,王为民.渤海冬季三维环流数值模拟.青岛海洋大学学报,1994,24(4):463~470.
[30]  周旭波,孙文心,苏键.东中国海潮余流自适应数值模拟.青岛海洋大学学报,2002,32(2):173~178.
[31]  江文胜,吴德星,高会旺.渤海夏季底层环流的观测与模拟.青岛海洋大学学报,2002,32(4):511~518.
[32]  Mellor G L,Yamada T1 A hierarchy of t urbulence clo sure models for planetary boundary layers1 J. At mo s. Sci.,1974,13:1791~1806.
[33]  Fang G,Yang J1 A t wo-dimensional numerical model of t he tidal motions in t he Bohai Sea1 Chinese Journal of Oceanology and Limnology,1985,3(2):135~152.
[34]  王凯,方国洪,冯士笮.渤海、黄海、东海M2潮汐潮流的三维数值模拟.海洋学报,1999,21(4):1~13.
[35]  Blumberg A F,Mellor G L. A description for a t hree2dimensional coastal ocean circulation model1 Heap s N S.(ed.). Three2Dimensional Coastal Models,Vol1 41 Washington D C:American Geop hysical U nion,1986.
[36]  Smagorinsky J. General circulation experiment s wit h t he primitive equations1 I:The basic experiment s. MonWeat her Rev.,1963,91:99~164.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133