Abstract
An adaptive grid dynamical core for a global atmospheric climate model has been developed. Adaptations allow a smooth transition from hydrostatic to non-hydrostatic physics at small resolution. The adaptations use a parallel program library for block-wise adaptive grids on the sphere. This library also supports the use of a reduced grid with coarser resolution in the longitudinal direction as the poles are approached. This permits the use of a longer time step since the CFL number restriction (CFL < 1) in a regular longitude-latitude grid is most severe in the zonal direction at high latitudes. Several tests show that our modelling procedures are stable and accurate.
| Original language | English |
|---|---|
| Pages (from-to) | 353-357 |
| Number of pages | 5 |
| Journal | Journal of Physics: Conference Series |
| Volume | 16 |
| Issue number | 1 |
| DOIs | |
| State | Published - Jan 1 2005 |
| Externally published | Yes |