Anisotropies occur naturally in computational fluid dynamics where the simulation of small-scale physical phenomena, such as boundary layers at high Reynolds numbers, causes the grid to be highly stretched, leading to a slowdown in convergence of multigrid methods. Several approaches aimed at making
Pseudo-time algorithms for the Navier-Stokes equations
β Scribed by R.C. Swanson; E. Turkel
- Publisher
- Elsevier Science
- Year
- 1986
- Tongue
- English
- Weight
- 856 KB
- Volume
- 2
- Category
- Article
- ISSN
- 0168-9274
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