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Luo Yiyong,Yu Guangyao,Huang Zuke. 1998. Numerical studies of upwelling in coastalareas of the East China Sea——Ⅰ The tide-induced upwelling. Acta Oceanologica Sinica, (1):15-25
Numerical studies of upwelling in coastalareas of the East China Sea——Ⅰ The tide-induced upwelling
Numerical studies of upwelling in coastalareas of the East China Sea——Ⅰ The tide-induced upwelling
Received:October 08, 1996  Revised:February 15, 1997
DOI:
Key words:East China Sea  tide-induced horizontal residual current  tide-induced upwelling  sea bottom topography with a steep slope
中文关键词:  East China Sea  tide-induced horizontal residual current  tide-induced upwelling  sea bottom topography with a steep slope
基金项目:This project was supported by the National Natural Science Foundation of China under contract No. 49136143.
Author NameAffiliation
Luo Yiyong Ocean University of Qingdao, Qingdao 266003, China 
Yu Guangyao Ocean University of Qingdao, Qingdao 266003, China 
Huang Zuke Ocean University of Qingdao, Qingdao 266003, China 
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Abstract:
      The M2 constituent in the coastal areas of the East China Sea is computed based on three-dimensional nonlinear tidal wave equations.The distributions of the tide-induced horizontal residual currents and the tide-induced vertical residual currents indicate that there exists a coastal upwelling stripe off Fujian and Zhejiang with a width of 40 km or so.The computed largest upwelling, 0.5×10-3 cm/s, occurs between 10 and 20 m levels.
中文摘要:
      The M2 constituent in the coastal areas of the East China Sea is computed based on three-dimensional nonlinear tidal wave equations.The distributions of the tide-induced horizontal residual currents and the tide-induced vertical residual currents indicate that there exists a coastal upwelling stripe off Fujian and Zhejiang with a width of 40 km or so.The computed largest upwelling, 0.5×10-3 cm/s, occurs between 10 and 20 m levels.
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