Gj. Hartke et D. Rind, IMPROVED SURFACE AND BOUNDARY-LAYER MODELS FOR THE GODDARD-INSTITUTE-FOR-SPACE-STUDIES GENERAL-CIRCULATION MODEL, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 102(D14), 1997, pp. 16407-16422
Improved surface and boundary layer models have been developed and imp
lemented in the Goddard Institute for Space Studies (GISS) general cir
culation model (GCM). The new boundary layer model retains the methodo
logy of the Model 2 version in which the surface winds are interpolate
d using a model profile but amends the approximations that were previo
usly used to keep the model analytical for ease of computation. The ne
w surface layer model is entirely different than that previously used
in the GISS GCM and uses similarity theory to compute the transport co
efficients, drag coefficient, Dalton number, and Stanton number. The c
ombination yields distinct improvements in the general circulation cha
racteristics of the GISS GCM. The new boundary layer and surface model
s were chosen to allow surface properties to be precomputed, resulting
in minimal impact to the overall execution time. This is particularly
important in a GCM used for climate experiments with timescales spann
ing centuries.