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Solution of nonlinear Stokes equations discretized by high-order finite elements on nonconforming and anisotropic meshes, with application to ice sheet dynamics

机译:用高阶有限差分离散非线性stokes方程的解   不合格和各向异性网格上的元素,适用于冰   表动态

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摘要

Motivated by the need for efficient and accurate simulation of the dynamicsof the polar ice sheets, we design high-order finite element discretizationsand scalable solvers for the solution of nonlinear incompressible Stokesequations. We focus on power-law, shear thinning rheologies used in modelingice dynamics and other geophysical flows. We use nonconforming hexahedralmeshes and the conforming inf-sup stable finite element velocity-pressurepairings $\mathbb{Q}_k\times \mathbb{Q}^\text{disc}_{k-2}$ or $\mathbb{Q}_k\times \mathbb{P}^\text{disc}_{k-1}$. To solve the nonlinear equations, wepropose a Newton-Krylov method with a block upper triangular preconditioner forthe linearized Stokes systems. The diagonal blocks of this preconditioner aresparse approximations of the (1,1)-block and of its Schur complement. The(1,1)-block is approximated using linear finite elements based on the nodes ofthe high-order discretization, and the application of its inverse isapproximated using algebraic multigrid with an incomplete factorizationsmoother. This preconditioner is designed to be efficient on anisotropicmeshes, which are necessary to match the high aspect ratio domains typical forice sheets. We develop and make available extensions to two libraries---ahybrid meshing scheme for the p4est parallel AMR library, and a modifiedsmoothed aggregation scheme for PETSc---to improve their support for solvingPDEs in high aspect ratio domains. In a numerical study, we find that oursolver yields fast convergence that is independent of the element aspect ratio,the occurrence of nonconforming interfaces, and of mesh refinement, and thatdepends only weakly on the polynomial finite element order. We simulate the iceflow in a realistic description of the Antarctic ice sheet derived from fielddata, and study the parallel scalability of our solver for problems with up to383M unknowns.
机译:由于需要高效,准确地模拟极地冰盖的动力学,我们设计了高阶有限元离散化和可扩展求解器来求解非线性不可压缩斯托克斯方程组。我们重点研究在模拟冰动力学和其他地球物理流中使用的幂律,剪切稀化流变学。我们使用不合格的六面体网格和合格的infsup稳定有限元速度-压力对$ \ mathbb {Q} _k \ times \ mathbb {Q} ^ \ text {disc} _ {k-2} $或$ \ mathbb {Q} _k \ times \ mathbb {P} ^ \ text {disc} _ {k-1} $。为了求解非线性方程,我们针对线性斯托克斯系统提出了带有块上三角前置条件的牛顿-克里洛夫方法。该预处理器的对角线块是(1,1)块及其Schur补的稀疏近似。 (1,1)块是根据线性高阶离散化的节点使用线性有限元来近似的,而其逆的应用是使用不完全因式分解平滑的代数多重网格来进行的。该预处理器被设计为在各向异性网格上有效,而各向异性网格是匹配典型模板的高纵横比域所必需的。我们开发并提供了对两个库的扩展-适用于p4est并行AMR库的混合网格划分方案和针对PETSc的改进的平滑聚合方案-来提高它们对解决高纵横比域中的PDE的支持。在数值研究中,我们发现求解器产生快速收敛,而收敛快速与元素长宽比,不合格界面的出现以及网格细化无关,并且仅微弱地依赖于多项式有限元顺序。我们在实际描述中根据现场数据得出的南极冰盖模拟了冰流,并研究了求解器对多达383M未知数问题的并行可扩展性。

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