浙闽沿岸潮余流的空间变化

林其良, 黄大吉, 宣基亮

海洋学研究 ›› 2015, Vol. 33 ›› Issue (4) : 30-36.

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海洋学研究 ›› 2015, Vol. 33 ›› Issue (4) : 30-36. DOI: 10.3969/j.issn.1001-909X.2015.04.003
研究论文

浙闽沿岸潮余流的空间变化

  • 林其良1,2, 黄大吉1,2,3, 宣基亮1,2
作者信息 +

Spatial variation of the tidal residual currents in the coastal area off Zhejiang and Fujian Provinces in the East China Sea

  • LIN Qi-liang1,2, HUANG Da-ji1,2,3, XUAN Ji-liang1,2
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文章历史 +

摘要

利用非结构网格海洋环流模式(FVCOM),研究了浙闽沿岸潮余流的空间变化及其生成机制。结果表明,浙闽沿岸的潮余流具有明显的水平二维特征。根据潮余流的流速和方向,浙闽沿岸的潮余流可分为3个区域,自东北向西南,依次为区域I、区域II和区域III。区域I和区域III的潮余流较强,前者流速为0.6~2.5 cm/s,方向沿等深线指向西南;后者流速为0.5~1.5 cm/s,方向沿等深线指向东北。区域II的潮余流较弱,均小于0.6 cm/s,方向自岸向海逆时针旋转,离岸较近区域方向指向西南,离岸较远区域方向指向东北。结合浙闽沿岸的潮余流和海底地形进行分析,发现潮余流与地形β效应ddx1H成正比,这与前人研究获得的海底地形对潮流的整流机制相符合,表明浙闽沿岸海域陡峭的海底地形对潮流有明显的整流作用。

Abstract

A detailed spatial structure of the tidal residual currents (TRCs) in the coastal area off Zhejiang and Fujian Provinces in the East China Sea was simulated by an unstructured grid-volume, three-dimensional, primitive equations ocean model (FVCOM). The simulated TRCs have apparent horizontal 2-D characters. The TRCs were further divided into three regions from north to south according to their velocity and direction, i.e., Region I, Region II and Region III. The TRCs in Region I and Region III are stronger but in opposite direction, flowing along isobaths in the southwestward with a velocity of 0.6~2.5 cm/s and northeastward directions with a velocity of 0.5~1.5 cm/s, respectively. The TRCs in Region II are weaker (less than 0.6 cm/s), and their directions are unticlockwise with the distance away from the coast. The analysis shows that the TRCs are directly proportional to the topographic beta factor ddx1H, this is consistent with the previous studies, and indicates the rectification of tidal currents when they flow over the steep bottom topography.

关键词

数值模拟 / 潮余流 / 地形β效应 / 浙闽沿岸

Key words

numerical simulation / tidal residual currents / topographic beta factor / coastal area off Zhejiang and Fujian Provinces

引用本文

导出引用
林其良, 黄大吉, 宣基亮. 浙闽沿岸潮余流的空间变化[J]. 海洋学研究. 2015, 33(4): 30-36 https://doi.org/10.3969/j.issn.1001-909X.2015.04.003
LIN Qi-liang, HUANG Da-ji, XUAN Ji-liang. Spatial variation of the tidal residual currents in the coastal area off Zhejiang and Fujian Provinces in the East China Sea[J]. Journal of Marine Sciences. 2015, 33(4): 30-36 https://doi.org/10.3969/j.issn.1001-909X.2015.04.003
中图分类号: P731   

参考文献

[1] PRANDLE D. Estuaries: Dynamics, mixing, sedimentation, and morphology [M]. Cambridge :Cambridge University Press,2009:236.
[2] LODER J W. Topographic rectification of tidal currents on the sides of Georges Bank [J]. J Phys Oceanogr,1980,10(9):1 399-1 416.
[3] HUTHNANCE J M. Tidal current asymmetries over the Norfolk Sandbanks [J]. Estuarine and Coastal Mar Sci,1973,I(1):89-99.
[4] HUTHNANCE J M. On mass transports generated by tides and long waves [J]. J Fluid Mec,1981,10(2):367-387.
[5] ZIMMERMAN J T F. Topographic generation of residual circulation by oscillatory (tidal) currents [J]. Geopnys Astrophys Fluid Dyn,1978,II(1):35-47.
[6] ZIMMERMAN J T F. Dynamics, diffusion and geomorphological significance of tidal residual eddies [J]. Nature,1981,290(5807):549-555.
[7] ROBINSON I S. Tidal vorticity and residual circulation [J]. Deep Sea Res,1980,28(81):195-212.
[8] ROBINSON I S. Tidally induced residual flows [M]//JOHNS B. Physical oceanography of coastal and shelf seas. Elsevier Oceanogr Ser,1983:321-356.
[9] MASS L R M, ZIMMERMAN J T F. On the exact shape of the horizontal profile of a topographically rectified tidal flow [J]. Geophys Fluid Dyn,1987,38(2):105-129.
[10] WRIGHT D G, LODER J W. On the influence of nonlinear bottom friction on the topographic rectification of tidal currents[J]. Geophys Astrophys Fluid Dyn,1988,42(3):227-245.
[11] MAZE R, LANGLOIS G, GROSJEAN F. Tidal eulerian residual currents over a slope: analytical and numerical frictionless models [J]. J Phys Oceagnogr,1998,28(7):1 321-1 332.
[12] MAZE R. Tidal rectification: friction or not friction [J]? J Phys Oceagnogr,1998,28(7):1 333-1 345.
[13] LODER J W, WRIGHT D G. Tidal rectification and frontal circulation on the sides of Georges Bank [J]. J Mar Res,1985,43(3):581-604.
[14] MASS L R M, ZIMMERMAN J T F. Tide-topography interactions in a stratified of shelf sea, I: Basic equations for quasi-nonlinear internal tides [J]. Geopnys Astrophys Fluid Dyn,1989a,45(1):1-35.
[15] MASS L R M, ZIMMERMAN J T F. Tide-topography interactions in a stratified of shelf sea, II: Bottom trapped internal tides and baroclinic residual currents [J]. Geopnys Astrophys Fluid Dyn, 1989b,45(1):37-69.
[16] CHEN Chang-sheng, BEARDSLEY R C. A numerical study of stratified tidal rectification over finite amplitude banks. Part I: Symmetric Banks [J]. J Phys Oceanogr,1995,25(9):2 090-2 110.
[17] CHEN Chang-sheng, BEARDSLEY R C, LIMEBURNER R. A numerical study of stratified tidal rectification over finite-amplitude banks. Part II: Georges Bank [J]. J Phys Oceanogr,1995,25(9):2 111-2 128.
[18] ZHAO Bao-ren, FANG Guo-hong, CAO De-ming. Characteristics of tidal residual currents and its relation to the near-shore circulation in the Bohai, the Yellow Sea and the East China Sea[J]. Studia Marina Sinica,1995,36(00): 1-11.
赵保仁,方国洪,曹德明.渤海、黄海和东海的潮余流特征及其与近岸环流输送的关系[J].海洋科学集刊,1995,36(00):1-11.
[19] WANG Kai, FENG Shi-zuo, SHI Xin-hui. A 3-D baroclinic model of summer circulation in the Bohai Sea, Yellow Sea and East China Sea[J]. Oceanol Limnol Sin,2001,32(5):551-560.
王凯,冯士筰,施心慧.渤、黄、东海夏季环流的三维斜压模型[J].海洋与湖沼,2001,32(5):551-560.
[20] QIAO Fang-li, ZHAO Wei, YUAN Ye-li. The research of the tidal long-term mass transport in the Bohai Sea, Yellow Sea and East China Sea[J]. Prog Nat Sci,2004,14(11):1 265-1 271.
乔方利,赵伟,袁业立.渤黄东海潮流长期物质输运研究[J].自然科学进展,2004,14(11):1 265-1 271.
[21] CHEN Qian, HUANG Da-ji, ZHANG Ben-zhao, et al. Characteristics of the tidal current and residual current in the seas adjacent to Zhejiang[J]. Donghai Mar Sci,2003a,21(4):1-14.
陈倩,黄大吉,章本照,等.浙江近海潮流和余流的特征[J].东海海洋,2003,21(4):1-14.
[22] CHEN Qian, HUANG Da-ji, ZHANG Ben-zhao. Numerical simulation of tide and tidal currents in the seas adjacent to Zhejiang[J]. Acta Oceanol Sin,2003b,25(5):9-20.
陈倩,黄大吉,章本照.浙江近海潮汐潮流的数值模拟[J]. 海洋学报,2003,25(5):9-20.
[23] DOU Zhen-xing, LUO Yuan-quan, HUANG Ke-xin, et al. Numerical computation of tidal current and tide-induced residual circulation in the Bohai Sea, Yellow Sea and East China sea[J]. Acta Oceanol Sin,1981,3(3):335-369.
窦振兴,罗远诠,黄克辛,等.渤、黄、东海潮流及潮余流的数值计算[J].海洋学报,1981,3(3):335-369.
[24] ZHAO Bao-ren, FANG Guo-hong, CAO De-ming. Numerical study on the tides and tidal currents in Bohai Sea, Yellow Sea and East China Sea[J]. Acta Oceanol Sin,1994,16(5):1-10.
赵保仁,方国洪,曹德明.渤、黄、东海潮汐潮流的数值模拟[J].海洋学报,1994,16(5):1-10.
[25] ZHU Xue-ming, BAO Xian-wen, SONG De-hai, et al. Numerical study on the tides and tidal currents in Bohai Sea, Yellow Sea and East China Sea[J]. Oceanol Limnol Sin,2012,43(6):1 103-1 113.
朱学明,鲍献文,宋德海,等.渤、黄、东海潮汐、潮流的数值模拟与研究[J].海洋与湖沼,2012,43(6):1 103-1 113.
[26] CHEN Chang-sheng, LIU He-dong, BEARDSLEY R C. An unstructured grid-volume, three-dimensional, primitive equations ocean model: application to coastal and estuaries [J]. J Atmos Oceanic Technol,2003,20(1):159-186.
[27] XUAN Ji-liang, YANG Zhao-qing, HUANG Da-ji, et al. Tidal residual current and its role in the mean flow on the Changjiang Bank[J]. J Mar Syst,2016,154A:66-81.

基金

国家重点基础研究发展计划项目资助(2011CB409803);国家自然科学基金项目资助(41306025);国家海洋公益性行业科研专项经费项目资助(201205015)

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