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Bai Yuchuan, Yu Tianyi. Split step and layered quasi-three-dimensional mathematical model of flow and its application to tide current calculation in the Lianzbou Bay[J]. Haiyang Xuebao, 1998, 20(5): 126-135.
Citation: Bai Yuchuan, Yu Tianyi. Split step and layered quasi-three-dimensional mathematical model of flow and its application to tide current calculation in the Lianzbou Bay[J]. Haiyang Xuebao, 1998, 20(5): 126-135.

Split step and layered quasi-three-dimensional mathematical model of flow and its application to tide current calculation in the Lianzbou Bay

  • Received Date: 1996-04-27
  • Rev Recd Date: 1997-05-06
  • Based on Navier-Stokes equation, the model equation has been deduced through algebraic coordinate transformation, then under this coordinate, the three-dimensional flow field is split into many layers along its depth and the model equation in each layer is integrated. As to numerical solving method, split step characteristic difference approximation and Galerkin lumping coefficient matrix definite element method are utilized. In a practical application,three-dimensional calculation to the tide current in the Lianzhou Bay, Zhuang Autonomous Region of Guangxi is done.
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  • 林乘南,黄菊卿,李新春.钱塘江河口潮流输沙数学模型.泥沙研究,1981, (2):16-27
    周建军,林乘南,王连祥.平面二维泥沙数学模型研究及应用.水利学报,1993, (11):10-19
    曹祖德,王桂芬.波浪掀沙、潮流输沙的数值模拟.海洋学报,1993, 15(1):107-118
    吴江航,韩庆书.计算流体力学的理论、方法及应用.北京:科学出版社,1988
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