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Stream function wave theory with a coflowing uniform current
Abstract Numerical stream function (Fourier) solutions for several waves in shallow, through intermediate to deep waters with a coflowing current or mass flux are presented in this paper. These solutions are calculated essentially from the previous algorithm of (Huang, M. C., Kinematic predictions by Stokes and Fourier wave theories. J. Waterway, Port, Coast & Ocean Enging, ASCE 116(1) (1990) 388-96.) where the unknown stream function coefficients are solved in a least-square approximation to the free surface boundary condition errors. The algorithm is further improved in this study to accommodate an incremental order procedure for shallow water waves, in order to avoid the mathematically correct but physically invalid triple-crested wave predictions. The characteristic features and predictive capabilities of this algorithm are discussed.
Stream function wave theory with a coflowing uniform current
Abstract Numerical stream function (Fourier) solutions for several waves in shallow, through intermediate to deep waters with a coflowing current or mass flux are presented in this paper. These solutions are calculated essentially from the previous algorithm of (Huang, M. C., Kinematic predictions by Stokes and Fourier wave theories. J. Waterway, Port, Coast & Ocean Enging, ASCE 116(1) (1990) 388-96.) where the unknown stream function coefficients are solved in a least-square approximation to the free surface boundary condition errors. The algorithm is further improved in this study to accommodate an incremental order procedure for shallow water waves, in order to avoid the mathematically correct but physically invalid triple-crested wave predictions. The characteristic features and predictive capabilities of this algorithm are discussed.
Stream function wave theory with a coflowing uniform current
Huang, Min-Chih (author)
Applied Ocean Research ; 14 ; 159-164
1992-02-05
6 pages
Article (Journal)
Electronic Resource
English
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