Conservative multidimensional upwinding for the steady two-dimensional shallow water equations

From MaRDI portal
Publication:1383022

DOI10.1006/jcph.1997.5823zbMath0902.76065OpenAlexW2024356719MaRDI QIDQ1383022

D. Massart

Publication date: 10 December 1998

Published in: Journal of Computational Physics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1006/jcph.1997.5823




Related Items (16)

Unsteady free surface flow simulation over complex topography with a multidimensional upwind technique.Streamline upwind Petrov-Galerkin methods for the steady-state Boltzmann transport equationUnconditionally stable space-time discontinuous residual distribution for shallow-water flowsApplication of conservative residual distribution schemes to the solution of the shallow water equations on unstructured meshesOn the accuracy of one-dimensional models of steady converging/diverging open channel flowsUnstructured finite volume discretisation of bed friction and convective flux in solute transport models linked to the shallow water equationsHigher order cell-based multidimensional upwind schemes for flow in porous media on unstructured gridsMultidimensional upwind schemes and higher resolution methods for three-component two-phase systems including gravity driven flow in porous media on unstructured gridsContinuous elliptic and multi-dimensional hyperbolic Darcy-flux finite-volume methodsResidual distribution for general time-dependent conservation lawsStabilized residual distribution for shallow water simulationsMulti-dimensional wave-oriented upwind schemes with reduced cross-wind diffusion for flow in porous mediaMultidimensional slope limiters for MUSCL-type finite volume schemes on unstructured gridsAn entropy-stable residual distribution scheme for the system of two-dimensional inviscid shallow water equationsConservative upwind difference schemes for the shallow water equationsConservative upwind difference schemes for the Euler equations



Cites Work


This page was built for publication: Conservative multidimensional upwinding for the steady two-dimensional shallow water equations