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南海环流动力机制研究综述

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Keywords: 南海,环流,中尺度涡,黑潮,吕宋海峡,东沙海流

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Abstract:

南海的环流复杂,但通过近20a来的研究工作,国内外学者对此已取得了不少的成果.本文就南海环流框架性的问题,综述了有关的文献,认为对南海上层海洋三方面的环流分量的驱动机制已有了初步的认识.这三方面分别是:(1)准季节性风场;(2)黑潮向南海的净输运;(3)黑潮向南海的涡度平流输送.但是对这些驱动的时空变化仍相当不清楚.三者皆增强了南海北部的海盆尺度气旋式环流,其强化的西南向西边界流靠近东沙群岛,建议称为“东沙海流”.没有水文证据显示黑潮水是以分支形式进入南海,其向南海的输运也不可能主要通过中尺度涡过程,具体机制有待研究.每年在南海生成的中尺度涡平均约有10个,风场与沿岸地形所生成的强风应力旋度可能是其主要的驱动机制.作为框架性的认识,也有三方面的工作进行得较少,即:(1)吕宋海峡的上层水交换;(2)南海的中尺度涡生成机制,虽然强风应力旋度及前述的第三种环流驱动机制也有中尺度涡伴生;(3)自吕宋海峡进入的深层水对南海上层海洋环流的影响.

References

[1]  SU Ji-lan , GUAN Bing xian, JLANG Jing-zhong.. The Kuroshio. Part I. Physical features[J]. Oceanography and Marine Biology: An Annual Review, 1990, 28: 11-71.
[2]  SU Ji-lan. Overview of the South China Sea circulation and its influence on the coastal physical oceanography outside the Pearl River Estu ary[J]. Continental Shelf Research, 2004, 24:1 745-1 760.
[3]  EMERY W J, DEWAR J S. Mean TS, SZ and TZ curve for the North Atlantic and the North Pacific[J]. Progress of Oceanography, 1982,11:219-305.
[4]  Chen C T A, Wang S L, Wang B J,et al. Nutrients budgets for the South China Sea basin[J]. Marine Chemistry,2001, 75:281-300.
[5]  QU T D, MITSUDERA T, YAMAGATA T. Intrusion of the North Pacific waters into the South China Sea[J]. Journal of Geophysical Research,2000, 105(C3):6 415-6 424.
[6]  CHU T Y. A study on the water exchange between Pacific Ocean and the South China Sea[J]. Acta Oceanographic Taiwanica, 1972, 2:11-24.
[7]  许建平,苏纪兰,仇德忠.黑潮水入侵南海的水文分析[A].中国海洋学文集6[C],2001.1-12.
[8]  SHAW P T. The seasonal variation of the intrusion of the Philippine Sea Water into the South China Sea[J]. Journal of Geophysical Research, 1991, 96:821-827.
[9]  METZGER E J, HURLBURT H. The importance of high horizontal resolution and accurate coastline geometry in modeling South China Sea inflow[J]. Geophysical Research Letters, 2001,28: 1 059-1 062.
[10]  WANG Gui-hua, SU Ji-lan,ChU P C. Mesoscale eddies in the South China Sea observed with altimeter data[J]. Geophysical Research Letters,2003, 30(21): 2121, doi: 10. 1029/2003GL018532.
[11]  CENTURIONI L R, NIILER P P, LEE D Y. Observations of inflow of Philippine Sea water into the South China Sea through the Luzon Strait[J]. Journal of Physical Oceanography, 2004, 34: 113-121.
[12]  徐锡祯,邱章,陈惠昌.南海水平环流的概述[A].中国海洋湖沼学会水文气象学会学术会议(1980)论文集[C].北京:科学出版社,1982.137-145.
[13]  KUO N J, ZHENG Q A, HO C R. Satellite observation of upwelling along the western coast of the South China Sea[J]. Remote Sensing of Environment, 2000, 74 : 463-470.
[14]  CHU P C, FAN C W, LOZANO C J, et al. An airborne expendable bathythermograph survey of the South China Sea, May 1995[J].Journal of Geophysical Research,1998, 103:21 637-21 652.
[15]  POHLMANN T. A three-dimensional circulation model of the South China Sea[A]. NIHOUL J J, JAMART B M. Three-dimensional Models of Marine and Estuarine Dynamics[M]. New York:Elsevier, 1987. 245-268.
[16]  LIU Z Y, YANG H J, LIU Q Y. Regional dynamics of seasonal variability in the South China Sea[J]. Journal of Physical Oceanography,2001, 31: 272-284.
[17]  苏纪兰,王卫.南海域台湾暖流源地问题[J].东海海洋,1990,8(3):1-9.
[18]  梁必骐.南海热带大气环流系统[M].北京:气象出版社,1991.244.
[19]  SU Ji lan. Circulation dynamics of the China Seas: north of 18°N[A]. Robinson A R, Brink K. The Sea, Vol. 11, The Global Coastal Ocean: Regional Studies and Syntheses[M]. John Wiley, 1998. 483-506.
[20]  刘增宏,许建平,李磊,等.1998年夏冬季节的南海水团和及其分布[A].中国海洋学文集13[C],2001.221-230.
[21]  杨跃红,李立,王肇鼎.南海的平均T-S、S-Z、T-Z特性[J].热带海洋,1988,7(3):54-59.
[22]  NITANI H. Beginning of the Kuroshio[A]. Stommel H, Yoshid a K. Kuroshio: Its Physical Aspects[M]. Seattle: University of Washington Press, 1972. 129 -163.
[23]  Chen C T A, Huang M H.. A mid depth front separating the South China Sea Water and the Philippine Sea WaterJ]. Journal of Oceanography,1996, 52:17 25.
[24]  袁耀初,刘勇刚,楼如云,等.2002年春季吕宋海峡海流:观测与改进逆模式计算[J].海洋学报,2005,27(3):1-10.
[25]  FANG G H, ZHAO B R, ZHU Y H. Water volume transport through the Taiwan Strait and the continental shelf of the East China Sea measured with current meters[J]. Oceanography of Asian Marginal Seas, Elsevier Oceanography Series, 1991, 54:345*358.
[26]  METZGER E J, HURLBURT H. Coupled dynamics of the South China Sea, Sulu Sea, and the Pacific Ocean[J]. Journal Geophysical Research,1996, 101:12 331 12 352.
[27]  GODFREY J S. A Sverdrup model of the depth-integrated flow for the world ocean allowing for island circulations[J]. Geophysical and Astrophysical Fluid Dynamics,1989, 45:89-112.
[28]  QU T D. Upper-layer circulation in the South China Sea[J]. Journal of Physical Oceanography,2000, 30:1 450-1 460.
[29]  南海综合调查报告.1979-1982南海北部多学科研究报告,第二卷[R].北京:科学出版社,1985.432.
[30]  苏纪兰.中国近海的环流动力机制研究[J].海洋学报,2001,23(4):1-16.
[31]  LI Li, NOWLIN W D, SU Ji-lan. Anticyclonic rings from the Kuroshio in the South China Sea[J]. Deep-Sea Research, Part Ⅰ, 1998, 45:1 469-1 482.
[32]  SHAW P T. The intrusion of water masses into the sea southwest of Taiwan[J]. Journal of Geophysical Research, 1989, 94:18 213-18 226.
[33]  PICHEVIN T, NOF D. The momentum imbalance paradox[J]. Tellus,1997, 49: 298-319.
[34]  王胄,陈庆生.南海东北部海域次表层水与中层水之流径[J].热带海洋,1997,16(2):24-41.
[35]  WYRTKI K. Scientific results of marine investigation of the South China Sea and Gulf of Thailand[A]. NAGA Report 2[R], 1961. 195.
[36]  HO C R, ZHENG Q A, SOONG Y S, et al. Seasonal variability of sea surface height in the South China Sea observed with TOPEX/Poseidon altimeter data[J]. Journal of Geophysical Research,2000, 105:13 981-13 990.
[37]  WANG L P, KOBLINSKY C J, HOWDEN S. Mesoscale variability in the South China Sea from the TOPEX/Poseidon altimetry data[J]. Deep-Sea Research, Part Ⅰ,2000, 47: 681-708.
[38]  王桂华.南海中尺度涡的运动规律探讨[D].青岛:中国海洋大学,2004.
[39]  XIE S P, XIE Q, WANG D X, et al. Summer upwelling in the South China Sea and its role in regional climate variations[J]. Journal of Geophysical Research, 2003, 108(C8): 3261, doi: 10. 1029/2003JC001876.
[40]  SHAW P T, CHAOS Y. Surface circulation in the South China Sea[J]. Deep-Sea Research, 1994, 41:1 663-1 683.
[41]  CESSI P, PRIMEAU F. Dissipative selection of low-frequency modes in a reduced-gravity basin[J]. Journal of Physical Oceanography,2001, 31: 127-137.
[42]  CESSI P, LOUAZEL S. Decadal oceanic response to stochastic wind forcing[J]. Journal of Physical Oceanography, 2001, 31: 3 020-3 029.
[43]  刘先炳,苏纪兰.南海环流的一个约化模式[J].海洋与湖沼,1992,23:167-174.
[44]  CAI Shu-quen,SU Ji-lan, GAN, Zi-jun, et al. The numerical study of the South China Sea upper circulation characteristics and its dynamic mechanism in winter[J]. Continental Shelf Research,2002, 22:2 247-2 264.

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