AN ALGORITHM FOR THE RESOLUTION OF CONDUCTION CONVENCTION BOUNDARY LAYERS
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.
Bibliographic Reference: REPORT IPP-5/18, 1988, AVAILABILITY: MAX-PLANCK-INSTITUT, MUENCHEN, D
Record Number: 1989126097800 / Last updated on: 1989-05-01
Available languages: en