2013
DOI: 10.1093/imanum/drt016
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A stabilized finite element method for advection-diffusion equations on surfaces

Abstract: Hybrid discontinuos Galerkin methods are popular discretization methods in applications from fluid dynamics and many others. Often large scale linear systems arising from elliptic operators have to be solved. We show that standard p-version domain decomposition techniques can be applied, but we have to develop new technical tools to prove poly-logarithmic condition number estimates, in particular on tetrahedral meshes.

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Cited by 60 publications
(52 citation statements)
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References 36 publications
(49 reference statements)
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“…Stabilization for advection-diffusion applications on manifolds were considered in the work of Olshanskii and Reusken. 34 The numerical results show that higher-order convergence rates are achieved provided that the finite element spaces are properly chosen. In addition, the conditioning of the system of equations depends on the element orders employed for the approximation of the individual physical fields.…”
Section: Introductionmentioning
confidence: 92%
“…Stabilization for advection-diffusion applications on manifolds were considered in the work of Olshanskii and Reusken. 34 The numerical results show that higher-order convergence rates are achieved provided that the finite element spaces are properly chosen. In addition, the conditioning of the system of equations depends on the element orders employed for the approximation of the individual physical fields.…”
Section: Introductionmentioning
confidence: 92%
“…Some different choices can be found in other works. 6,24,29,33,46,47 The stabilization parameter used in this paper is a combination of the strategies from the works of Elman et al 29 and Roos et al, 33 ie, using the gradually changing parameter for different regions according to their local mesh Peclet numbers.…”
Section: The Sdmmentioning
confidence: 99%
“…Convection-diffusion-reaction partial differential equations (PDEs) on surfaces are intensively applied to model the transport or migration processes in physical and biological science. Well-known application examples are the transport of surfactants on moving interfaces with application to multiphase flows [1][2][3][4][5][6] and the chemotaxis processes in which single colonies of bacteria cells merge together to form one larger colony on solid surfaces and biological films. [7][8][9][10] Surface convection and diffusion problems are also fundamental subproblems involved in the surface flow models with applications to geoscience.…”
Section: Introductionmentioning
confidence: 99%
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