Dp. Kratz et al., Minor trace gas radiative forcing calculations using the k distribution method with one-parameter scaling, J GEO RES-A, 103(D24), 1998, pp. 31647-31656
The k distribution method with one-parameter pressure and temperature scali
ng, first developed for water vapor, has now been applied to the minor trac
e gas (N2O, CH4, CFCs, and two minor bands of CO2) absorption in the infrar
ed window region (800-1380 cm(-1)). The derivation of the k distributions i
s based upon an exponential sum fitting to the monochromatically calculated
transmission functions at a predetermined reference pressure and temperatu
re. For nonhomogeneous path lengths, one-parameter scaling is utilized in c
onjunction with the k distribution method. To determine the accuracies of t
he k distribution method as compared to the monochromatic calculations, flu
xes and cooling rates are calculated for a wide variety of atmospheric cond
itions. For the entire 800-1380 cm(-1) spectral range the effect of the min
or trace gases on the fluxes calculated using the k distribution method is
within 2.3% of the monochromatic method. In addition to being accurate, thi
s method is computationally very fast. When implemented into the Goddard EO
S general circulation model, the computing time for the longwave flux calcu
lations is increased by only 20% despite the inclusion of the minor trace g
as absorption bands.