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Abstract

A finite difference time-dependent algorithm for the steady-state solution of conduction-convection problems is discussed. The scheme is applied to a boundary layer problem; in the region where steep gradients occur a higher grid resolution is used. The accumulated mesh is mapped to an equidistant grid by a suitable space- transformation. A corresponding time-transformation has the potential to reduce the computational effort.

Additional information

Authors: ZANINO R, IPP, D;LACKNER K, IPP, D;SCHNEIDER W IPP, D, IPP, D
Bibliographic Reference: REPORT IPP-5/18, 1988, AVAILABILITY: MAX-PLANCK-INSTITUT, MUENCHEN, D
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