Scaling to the stars -- a linearly scaling elliptic solver for $p$-multigrid
Autor: | Jochen Fröhlich, Jörg Stiller, Immo Huismann |
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Rok vydání: | 2018 |
Předmět: |
Physics and Astronomy (miscellaneous)
Degrees of freedom (statistics) Inverse FOS: Physical sciences 010103 numerical & computational mathematics Residual 01 natural sciences Multigrid method Operator (computer programming) FOS: Mathematics Applied mathematics Degree of a polynomial Mathematics - Numerical Analysis 0101 mathematics Scaling Mathematics Numerical Analysis Applied Mathematics Numerical Analysis (math.NA) Solver Computational Physics (physics.comp-ph) Computer Science Applications 010101 applied mathematics Computational Mathematics Modeling and Simulation Physics - Computational Physics |
DOI: | 10.48550/arxiv.1808.03595 |
Popis: | High-order methods gain increased attention in computational fluid dynamics. However, due to the time step restrictions arising from the semi-implicit time stepping for the incompressible case, the potential advantage of these methods depends critically on efficient elliptic solvers. Due to the operation counts of operators scaling with the polynomial degree p times the number of degrees of freedom n DOF , the runtime of the best available multigrid solvers scales with O ( p ⋅ n DOF ) . This scaling with p significantly lowers the applicability of high-order methods to high orders. While the operators for residual evaluation can be linearized when using static condensation, Schwarz -type smoothers require their inverses on fixed subdomains. No explicit inverse is known in the condensed case and matrix-matrix multiplications scale with p ⋅ n DOF . This paper derives a matrix-free explicit inverse for the static condensed operator in a cuboidal, Cartesian subdomain. It scales with p 3 per element, i.e. n DOF globally, and allows for a linearly scaling additive Schwarz smoother, yielding a p-multigrid cycle with an operation count of O ( n DOF ) . The resulting solver uses fewer than four iterations for all polynomial degrees to reduce the residual by ten orders and has a runtime scaling linearly with n DOF for polynomial degrees at least up to 48. Furthermore the runtime is less than one microsecond per unknown over wide parameter ranges when using one core of a CPU, leading to time-stepping for the incompressible Navier-Stokes equations using as much time for explicitly treated convection terms as for the elliptic solvers. |
Databáze: | OpenAIRE |
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