next up previous contents
Next: 29.3.2.3 Non-divergent barotropic velocities Up: 29.3.2 Remarks Previous: 29.3.2.1 Boundary conditions

29.3.2.2 Conditioning of the elliptic operator

The second point to be made is that Equation (29.39) contains a factor Hi,jrow whereas the elliptic equation for the stream function contains the factor 1/Hi,jrow which should make this method less prone to stability problems than the stream function equation when topography contains steep slopes.



RC Pacanowski and SM Griffies, GFDL, Jan 2000