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A Discontinuous Galerkin Method for Three-Dimensional Shallow Water Equations

Clint  DawsonContact Information and Vadym  Aizinger1

(1) Center for Subsurface Modeling - C0200, Institute for Computational Engineering and Sciences (ICES), The University of Texas at Austin, Austin , TX 78712, USA

Received: 04 August 2003  Accepted: 25 February 2004  

Abstract  We describe the application of a local discontinuous Galerkin method to the numerical solution of the three-dimensional shallow water equations. The shallow water equations are used to model surface water flows where the hydrostatic pressure assumption is valid. The authors recently developed a DG\linebreak method for the depth-integrated shallow water equations. The method described here is an extension of these ideas to non-depth-integrated models. The method and its implementation are discussed, followed by numerical examples on several test problems.

Keywords  Shallow water equations - discontinuous Galerkin method - free surface

This revised version was published online in July 2005 with corrected volume and issue numbers.

Contact InformationClint  Dawson
Email: clint@ices.utexas.edu
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Referenced by
3 newer articles

  1. Restelli, Marco (2009) A Conservative Discontinuous Galerkin Semi-Implicit Formulation for the Navier–Stokes Equations in Nonhydrostatic Mesoscale Modeling. SIAM Journal on Scientific Computing 31(3)
    [CrossRef]
  2. Ern, A. (2007) A well-balanced Runge–Kutta discontinuous Galerkin method for the shallow-water equations with flooding and drying. International Journal for Numerical Methods in Fluids
    [CrossRef]
  3. (2005) Foreword. Journal of Scientific Computing 22-23(1-3)
    [CrossRef]
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