CENTRAL-DIFFERENCE AND UPWIND-BIASED SCHEMES FOR STEADY AND UNSTEADY EULER AEROFOIL COMPUTATIONS

Authors
Citation
Cb. Allen, CENTRAL-DIFFERENCE AND UPWIND-BIASED SCHEMES FOR STEADY AND UNSTEADY EULER AEROFOIL COMPUTATIONS, Aeronautical Journal, 99(982), 1995, pp. 52-62
Citations number
NO
Categorie Soggetti
Aerospace Engineering & Tecnology
Journal title
ISSN journal
00019240
Volume
99
Issue
982
Year of publication
1995
Pages
52 - 62
Database
ISI
SICI code
0001-9240(1995)99:982<52:CAUSFS>2.0.ZU;2-K
Abstract
Two numerical methods are presented for the computation of steady and unsteady Euler flows. These are applied to steady and unsteady flows a bout the NACA 0012 aerofoil, using structured grids generated by the t ransfinite interpolation technique. An explicit central-difference sch eme is produced based on the cell-vertex method of Ni modified by Hall . The method is second-order accurate in time and space, and with flow quantities stored at boundaries the boundary conditions are simple to apply. This is a definite advantage over the cell-centred approach of Jameson, where extrapolation of the flow quantities is required at th e boundaries, making unsteady boundary conditions difficult to apply. An explicit upwind-biased scheme is also produced, based on the flux-v ector splitting of van Leer. The method adopts a three stage Runge-Kut ta time-stepping scheme and a high-order spatial discretisation which is formally third-order accurate for one-dimensional calculations. The upwind scheme is shown to be slightly more accurate than the central- difference scheme for steady aerofoil flows, but it is not clear which is the more accurate for unsteady aerofoil hows. However, the central -difference scheme requires less than half the CPU time of the upwind- difference scheme, and hence is attractive, especially when considerin g three-dimensional flows. The transfinite interpolation technique is ideal for generating moving structured grids due to its simplicity, an d grid speeds are available algebraically by the same interpolation as grid points. The method is also ideal for use in a multiblock approac h.