NCAR Summer School, 13 August 2008
Regional Climate Models
Increased computing power has allowed finer resolution
Computing requirements increase inversely with cube of horizontal resolution: for example, if the grid spacing is cut in half,
"twice as many grid points are needed in each direction and
"twice as many time steps are needed to reach a given future time (because the maximum allowable time step varies about linearly with grid spacing).
1990
1996
2001
2007
[Note first:  GCMs use a planet divided into small regions (grid boxes) and compute their equations for each grid box.]
Figure 1.4. Geographic resolution characteristic of the generations of climate models used in the IPCC Assessment Reports: FAR (IPCC, 1990), SAR (IPCC, 1996), TAR (IPCC, 2001a), and AR4 (2007). The figures above show how successive generations of these global models increasingly resolved northern Europe. These illustrations are representative of the most detailed horizontal resolution used for short-term climate simulations. The century-long simulations cited in IPCC Assessment Reports after the FAR were typically run with the previous generationŐs resolution. Vertical resolution in both atmosphere and ocean models is not shown, but it has increased comparably with the horizontal resolution, beginning typically with a single-layer slab ocean and ten atmospheric layers in the FAR and progressing to about thirty levels in both atmosphere and ocean.