In this work, we compare and contrast two provably entropy stable and high-order accurate nodal discontinuous Galerkin spectral element methods applied to the one dimensional shallow water equations for problems with non-constant bottom topography. Of particular importance for numerical approximations of the shallow water equations is the well-balanced property. The well-balanced property is an attribute that a numerical approximation can preserve a steady-state solution of constant water height in the presence of a bottom topography. Numerical tests are performed to explore similarities and differences in the two high-order schemes
A space-time discontinuous Galerkin (DG) nite element method is presented for the shallow water equ...
The shallow-water equations (SWE), derived from the incompressible Navier-Stokes equations using the...
The shallow-water equations are widely used to model surface water bodies, such as lakes, rivers and...
In this work, we compare and contrast two provably entropy stable and high-order accurate nodal disc...
In this work, we design an arbitrary high order accurate nodal discontinuous Galerkin spectral eleme...
We design an arbitrary high-order accurate nodal discontinuous Galerkin spectral element approximati...
We design an arbitrary high-order accurate nodal discontinuous Galerkin spectral element approximati...
We extend the entropy stable high order nodal discontinuous Galerkin spectral element approximation ...
International audienceWe consider in this work the discontinuous Galerkin discretization of the nonl...
International audienceThis paper investigates a first-order and a second-order approximation techniq...
Abstract. In this paper, we survey our recent work on designing high order positivity-preserving wel...
Shallow-Water Equations are encountered in many applications related to hydraulics, flood propagatio...
Abstract The shallow water equations model flows in rivers and coastal areas and have wide applicati...
AbstractThe Lagrange-Galerkin spectral element method for the two-dimensional shallow water equation...
Abstract. We consider the shallow water equations with non-flat bottom topography. The smooth soluti...
A space-time discontinuous Galerkin (DG) nite element method is presented for the shallow water equ...
The shallow-water equations (SWE), derived from the incompressible Navier-Stokes equations using the...
The shallow-water equations are widely used to model surface water bodies, such as lakes, rivers and...
In this work, we compare and contrast two provably entropy stable and high-order accurate nodal disc...
In this work, we design an arbitrary high order accurate nodal discontinuous Galerkin spectral eleme...
We design an arbitrary high-order accurate nodal discontinuous Galerkin spectral element approximati...
We design an arbitrary high-order accurate nodal discontinuous Galerkin spectral element approximati...
We extend the entropy stable high order nodal discontinuous Galerkin spectral element approximation ...
International audienceWe consider in this work the discontinuous Galerkin discretization of the nonl...
International audienceThis paper investigates a first-order and a second-order approximation techniq...
Abstract. In this paper, we survey our recent work on designing high order positivity-preserving wel...
Shallow-Water Equations are encountered in many applications related to hydraulics, flood propagatio...
Abstract The shallow water equations model flows in rivers and coastal areas and have wide applicati...
AbstractThe Lagrange-Galerkin spectral element method for the two-dimensional shallow water equation...
Abstract. We consider the shallow water equations with non-flat bottom topography. The smooth soluti...
A space-time discontinuous Galerkin (DG) nite element method is presented for the shallow water equ...
The shallow-water equations (SWE), derived from the incompressible Navier-Stokes equations using the...
The shallow-water equations are widely used to model surface water bodies, such as lakes, rivers and...