On computing the three dimensional flow in a stratified sea using the Galerkin method
DOI10.1016/S0307-904X(82)80098-XzbMath0497.76018MaRDI QIDQ1170948
Publication date: 1982
Published in: Applied Mathematical Modelling (Search for Journal in Brave)
B-splinescirculation of stratified seadepth-varying functionseddy viscosity and densityexpansions for currents, density and internal displacement in terms of horizontally and time-varying coefficientsthree-dimensional linear equations
Probabilistic models, generic numerical methods in probability and statistics (65C20) Incompressible viscous fluids (76D99) Finite difference methods for boundary value problems involving PDEs (65N06) Galactic and stellar dynamics (85A05) Jets and cavities, cavitation, free-streamline theory, water-entry problems, airfoil and hydrofoil theory, sloshing (76B10) Basic methods in fluid mechanics (76M99)
Related Items (5)
Cites Work
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- On formulating a three-dimensional hydrodynamic sea model with an arbitrary variation of vertical eddy viscosity
- Three dimensional numerical sea model using the Galerkin method with a polynomial basis set
- Application of the Galerkin method to the formulation of a three- dimensional nonlinear hydrodynamic numerical sea model
- A numerical investigation of errors arising in applying the Galerkin method of the solution of nonlinear partial differential equations
- Application of the Galerkin method to the solution of Burgers' equation
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