The numerical solution of the non-stationary, incompressible Navier-Stokes model can be split into linearized auxiliary problems of Oseen type. We present in a unique way different stabilization techniques of finite element schemes on isotropic meshes. First we describe the state-of-the-art for the
An adaptive stabilized finite element method for the generalized Stokes problem
β Scribed by Rodolfo Araya; Gabriel R. Barrenechea; Abner Poza
- Publisher
- Elsevier Science
- Year
- 2008
- Tongue
- English
- Weight
- 713 KB
- Volume
- 214
- Category
- Article
- ISSN
- 0377-0427
No coin nor oath required. For personal study only.
β¦ Synopsis
In this work we present an adaptive strategy (based on an a posteriori error estimator) for a stabilized finite element method for the Stokes problem, with and without a reaction term. The hierarchical type estimator is based on the solution of local problems posed on appropriate finite dimensional spaces of bubble-like functions. An equivalence result between the norm of the finite element error and the estimator is given, where the dependence of the constants on the physics of the problem is explicited. Several numerical results confirming both the theoretical results and the good performance of the estimator are given.
π SIMILAR VOLUMES
## Abstract A new stabilized finite element method for the Stokes problem is presented. The method is obtained by modification of the mixed variational equation by using local __L__^2^ polynomial pressure projections. Our stabilization approach is motivated by the inherent inconsistency of equalβor
## a b s t r a c t Based on the lowest equal-order conforming finite element subspace (X h , M h ) (i.e. P 1 -P 1 or Q 1 -Q 1 elements), a characteristic stabilized finite element method for transient Navier-Stokes problem is proposed. The proposed method has a number of attractive computational p
A finite element discretization for two-dimensional MHD is described. The elements are triangles with piecewise linear basis functions. The main computational difficulty is the accurate calculation of the current. The most effective solution is to employ a current-vorticity advection formulation of