Proceedings of the International Conference for High Performance Computing, Networking, Storage and Analysis 2015
DOI: 10.1145/2807591.2807675
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An extreme-scale implicit solver for complex PDEs

Abstract: Mantle convection is the fundamental physical process within earth's interior responsible for the thermal and geological evolution of the planet, including plate tectonics. The mantle is modeled as a viscous, incompressible, non-Newtonian fluid. The wide range of spatial scales, extreme variability and anisotropy in material properties, and severely nonlinear rheology have made global mantle convection modeling with realistic parameters prohibitive. Here we present a new implicit solver that exhibits optimal a… Show more

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Cited by 103 publications
(32 citation statements)
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“…This greatly increases model run time and therefore it is important to implement a more efficient nonlinear solving strategy than the Picard iterations currently used by ASPECT. The more sophisticated Newton solver (see for example Popov and Sobolev, 2008;May et al, 2015;Rudi et al, 2015;Kaus et al, 2016;Wilson et al, 2017) will help achieve faster convergence. Convergence behavior has also been suggested to improve from including elasticity (Kaus, 2010), but especially dynamic pressure-dependent plasticity remains difficult to converge for both Picard iterations and Newton solvers (Spiegelman et al, 2016).…”
Section: Discussionmentioning
confidence: 99%
“…This greatly increases model run time and therefore it is important to implement a more efficient nonlinear solving strategy than the Picard iterations currently used by ASPECT. The more sophisticated Newton solver (see for example Popov and Sobolev, 2008;May et al, 2015;Rudi et al, 2015;Kaus et al, 2016;Wilson et al, 2017) will help achieve faster convergence. Convergence behavior has also been suggested to improve from including elasticity (Kaus, 2010), but especially dynamic pressure-dependent plasticity remains difficult to converge for both Picard iterations and Newton solvers (Spiegelman et al, 2016).…”
Section: Discussionmentioning
confidence: 99%
“…Multigrid is known for its mesh-independent convergence and optimal complexity in the number of unknowns Hackbusch (1985); Brandt and Diskin (1994). Therefore, parallel multigrid is of a special interest for large scale high-performance computations, Gmeiner et al (2016); Notay and Napov (2015); Sundar et al (2012); Rudi et al (2015). The mesh hierarchy T introduced in Section 2.1 is used to construct a geometric multigrid solver with its coarsest level for = 0 and finest level for = L. In order to solve the algebraic equation A L u L = f L associated with the finest mesh, we apply multigrid V-cycles; see, e.g, (Hackbusch, 1985, Algorithm (2.5.4)).…”
Section: Solver Setupmentioning
confidence: 99%
“…For example, in [16], an Earth's mantle convection flow solver based on highorder continuous/discontinuous finite elements with octree-based adaptive mesh refinement and coarsening (AMR/C) is reported to scale up to 1.5 million processor cores such strategy. The referred paper won the prestigious Gordon Bell prize in 2015.…”
Section: Introductionmentioning
confidence: 99%