Preconditioning the Advection-Diffusion Equation: the Green's Function Approach

We look at the relationship between efficient preconditioners (i.e., good approximations to the discrete inverse operator) and the generalized inverse for the (continuous) advection-diffusion operator -- the Green's function. We find that the continuous Green's function exhibits two import...

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Main Authors: Loghin, D, Wathen, A
Format: Report
Published: Unspecified 1997
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author Loghin, D
Wathen, A
author_facet Loghin, D
Wathen, A
author_sort Loghin, D
collection OXFORD
description We look at the relationship between efficient preconditioners (i.e., good approximations to the discrete inverse operator) and the generalized inverse for the (continuous) advection-diffusion operator -- the Green's function. We find that the continuous Green's function exhibits two important properties -- directionality and rapid downwind decay -- which are preserved by the discrete (grid) Green's functions, if and only if the discretization used produces non-oscillatory solutions. In particular, the downwind decay ensures the locality of the grid Green's functions. Hence, a finite element formulation which produces a good solution will typically use a coefficient matrix with almost lower triangular structure under a "with-the-flow" numbering of the variables. It follows that the block Gauss-Seidel matrix is a first candidate for a preconditioner to use with an iterative solver of Krylov subspace type.
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spelling oxford-uuid:94b480e7-0544-4735-8de8-23387688f4fe2022-03-26T23:41:18ZPreconditioning the Advection-Diffusion Equation: the Green's Function ApproachReporthttp://purl.org/coar/resource_type/c_93fcuuid:94b480e7-0544-4735-8de8-23387688f4feMathematical Institute - ePrintsUnspecified1997Loghin, DWathen, AWe look at the relationship between efficient preconditioners (i.e., good approximations to the discrete inverse operator) and the generalized inverse for the (continuous) advection-diffusion operator -- the Green's function. We find that the continuous Green's function exhibits two important properties -- directionality and rapid downwind decay -- which are preserved by the discrete (grid) Green's functions, if and only if the discretization used produces non-oscillatory solutions. In particular, the downwind decay ensures the locality of the grid Green's functions. Hence, a finite element formulation which produces a good solution will typically use a coefficient matrix with almost lower triangular structure under a "with-the-flow" numbering of the variables. It follows that the block Gauss-Seidel matrix is a first candidate for a preconditioner to use with an iterative solver of Krylov subspace type.
spellingShingle Loghin, D
Wathen, A
Preconditioning the Advection-Diffusion Equation: the Green's Function Approach
title Preconditioning the Advection-Diffusion Equation: the Green's Function Approach
title_full Preconditioning the Advection-Diffusion Equation: the Green's Function Approach
title_fullStr Preconditioning the Advection-Diffusion Equation: the Green's Function Approach
title_full_unstemmed Preconditioning the Advection-Diffusion Equation: the Green's Function Approach
title_short Preconditioning the Advection-Diffusion Equation: the Green's Function Approach
title_sort preconditioning the advection diffusion equation the green s function approach
work_keys_str_mv AT loghind preconditioningtheadvectiondiffusionequationthegreensfunctionapproach
AT wathena preconditioningtheadvectiondiffusionequationthegreensfunctionapproach