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High-order discontinuous element-based schemes for the inviscid shallow water equations: spectral multidomain penalty and discontinuous Galerkin methods

机译:无粘性浅水方程的基于高阶不连续元素的格式:谱多域罚和不连续Galerkin方法

摘要

Two commonly used types of high-order-accuracy element-based schemes, collocationbasedspectral multidomain penalty methods (SMPM) and nodal discontinuousGalerkin methods (DGM), are compared in the framework of the inviscid shallowwater equations. Differences and similarities in formulation are identified,with the primary difference being the dissipative term in the Rusanov form ofthe numerical flux for the DGM that provides additional numerical stability;however, it should be emphasized that to arrive at this equivalence betweenSMPM and DGM requires making specific choices in the construction of bothmethods; these choices are addressed. In general, both methods offer a multitudeof choices in the penalty terms used to introduce boundary conditionsand stabilize the numerical solution. The resulting specialized class of SMPMand DGM are then applied to a suite of six commonly considered geophysicalflow test cases, three linear and three non-linear; we also include results fora classical continuous Galerkin (i.e., spectral element) method for comparison.Both the analysis and numerical experiments show that the SMPM and DGMare essentially identical; both methods can be shown to be equivalent for veryspecial choices of quadrature rules and Riemann solvers in the DGM along withspecial choices in the type of penalty term in the SMPM. Although we onlyfocus our studies on the inviscid shallow water equations the results presentedshould be applicable to other systems of nonlinear hyperbolic equations (suchas the compressible Euler equations) and extendable to the compressible andincompressible Navier-Stokes equations, where viscous terms are included.
机译:在无粘性浅水方程的框架内,比较了两种常用的基于高阶精度元素的方案,即基于搭配的光谱多域惩罚方法(SMPM)和节点不连续伽勒金方法(DGM)。确定了配方上的差异和相似之处,主要区别是Rusanov形式的DGM数值通量的耗散项,它提供了额外的数值稳定性;但是,应强调的是,要达到SMPM和DGM之间的等价关系两种方法的选择;解决了这些选择。通常,这两种方法都在用于引入边界条件和稳定数值解的惩罚项中提供了多种选择。然后将生成的特殊类别的SMPM和DGM应用于一组六个通常被认为是地球物理流量的测试用例,其中三个是线性的,三个是非线性的;分析和数值实验均表明,SMPM和DGM基本相同;我们还提供了经典连续Galerkin(即光谱元素)方法的比较结果。对于DGM中的正交规则和Riemann求解器的非常特殊的选择,以及SMPM中惩罚项类型的特殊选择,这两种方法都可以等效。尽管我们仅将研究重点放在无粘性的浅水方程上,但给出的结果应适用于非线性双曲方程的其他系统(例如可压缩的Euler方程),并且可扩展到可压缩和不可压缩的Navier-Stokes方程,其中包括粘性项。

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