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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

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摘要

Two commonly used types of high-order-accuracy element-based schemes, collocation-based spectral multidomain penalty methods (SMPM) and nodal discontinuous Galerkin methods (DGM), are compared in the framework of the inviscid shallow water equations. Differences and similarities in formulation are identified, with the primary difference being the dissipative term in the Rusanov form of the numerical flux for the DGM that provides additional numerical stability; however, it should be emphasized that to arrive at this equivalence between SMPM and DGM requires making specific choices in the construction of both methods; these choices are addressed. In general, both methods offer a multitude of choices in the penalty terms used to introduce boundary conditions and stabilize the numerical solution. The resulting specialized class of SMPM and DGM are then applied to a suite of six commonly considered geophysical flow test cases, three linear and three non-linear; we also include results for a classical continuous Galerkin (i.e., spectral element) method for comparison. Both the analysis and numerical experiments show that the SMPM and DGM are essentially identical; both methods can be shown to be equivalent for very special choices of quadrature rules and Riemann solvers in the DGM along with special choices in the type of penalty term in the SMPM. Although we only focus our studies on the inviscid shallow water equations the results presented should be applicable to other systems of nonlinear hyperbolic equations (such as the compressible Euler equations) and extendable to the compressible and incompressible 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,即基于搭配的频谱多域惩罚方法(SMPM)和节点间断Galerkin方法(DGM)。确定配方上的差异和相似之处,主要区别是DGM数值通量的Rusanov形式中的耗散项,它提供了额外的数值稳定性;但是,应该强调的是,要实现SMPM和DGM之间的等效性,就需要在两种方法的构造中做出特定选择;解决了这些选择。通常,两种方法都在惩罚项中提供了多种选择,这些惩罚项用于引入边界条件并稳定数值解。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;我们还提供了经典连续Galerkin(即光谱元素)方法的结果进行比较。分析和数值实验都表明,SMPM和DGM本质上是相同的。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其他非线性双曲方程组(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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