A velocity-based moving mesh Discontinuous Galerkin method for the advection-diffusion equation
Ezra Rozier, Jörn Behrens
TL;DR
The paper addresses robust numerical solution of unsteady advection-diffusion problems in convection-dominated regimes by introducing a velocity-based moving mesh DG method. It splits the flow into a smooth mean motion $\tilde{\mathbf{V}}$ and a residual $\mathbf{V}-\tilde{\mathbf{V}}$, uses an ALE-DG formulation on a fixed reference domain, and derives both a priori and robust a posteriori error estimates for the semi-discrete scheme. Theoretical results show second-order spatial convergence when the remaining advection is small and the mesh-velocity is sufficiently regular, while the a posteriori estimators enable local refinement that remains reliable under large mesh Peclet numbers. Numerical tests on a boundary-layer problem confirm that the moving mesh focuses resolution where needed, maintaining stability and improving accuracy compared to static meshes with DG."
Abstract
In convection-dominated flows, robustness of the spatial discretisation is a key property. While Interior Penalty Galerkin (IPG) methods already proved efficient in the situation of large mesh Peclet numbers, Arbitrary Lagrangian-Eulerian (ALE) methods are able to reduce the convection-dominance by moving the mesh. In this paper, we introduce and analyse a velocity-based moving mesh discontinuous Galerkin (DG) method for the solution of the linear advection-diffusion equation. By introducing a smooth parameterized velocity $\Tilde{V}$ that separates the flow into a mean flow, also called moving mesh velocity, and a remaining advection field $V-\Tilde{V}$, we made a convergence analysis based on the smoothness of the mesh velocity. Furthermore, the reduction of the advection speed improves the stability of an explicit time-stepping. Finally, by adapting the existing robust error criteria to this moving mesh situation, we derived robust \textit{a posteriori} error criteria that describe the potentially small deviation to the mean flow and include the information of a transition towards $V=\Tilde{V}$.
