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Parallel finite element computation of unsteady incompressible flows
Author(s) -
Wasfy Tamer,
West Alan C.,
Modi Vijay
Publication year - 1998
Publication title -
international journal for numerical methods in fluids
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.938
H-Index - 112
eISSN - 1097-0363
pISSN - 0271-2091
DOI - 10.1002/(sici)1097-0363(19980115)26:1<17::aid-fld619>3.0.co;2-g
Subject(s) - reynolds number , computation , compressibility , mathematics , pressure correction method , finite element method , benchmark (surveying) , computational fluid dynamics , speedup , galerkin method , mathematical optimization , computer science , mechanics , physics , algorithm , parallel computing , turbulence , geodesy , thermodynamics , geography
A parallel semi‐explicit iterative finite element computational procedure for modelling unsteady incompressible fluid flows is presented. During the procedure, element flux vectors are calculated in parallel and then assembled into global flux vectors. Equilibrium iterations which introduce some ‘local implicitness’ are performed at each time step. The number of equilibrium iterations is governed by an implicitness parameter. The present technique retains the advantages of purely explicit schemes, namely (i) the parallel speed‐up is equal to the number of parallel processors if the small communication overhead associated with purely explicit schemes is ignored and (ii) the computation time as well as the core memory required is linearly proportional to the number of elements. The incompressibility condition is imposed by using the artificial compressibility technique. A pressure‐averaging technique which allows the use of equal‐order interpolations for both velocity and pressure, this simplifying the formulation, is employed. Using a standard Galerkin approximation, three benchmark steady and unsteady problems are solved to demonstrate the accuracy of the procedure. In all calculations the Reynolds number is less than 500. At these Reynolds numbers it was found that the physical dissipation is sufficient to stabilize the convective term with no need for additional upwind‐type dissipation. © 1998 John Wiley & Sons, Ltd.