The influence of spatially inhomogeneous water vapour distributions on the
solar radiative fluxes of inhomogeneous clouds has been estimated by means
of Monte Carlo radiative transfer calculations and line by line calculation
s for transmission at water vapour and oxygen. 96 cloud realizations obtain
ed by the atmospheric model GESIMA have been considered for the following c
ases: 1) Clouds embedded in a 3d inhomogeneous gas atmosphere and 2) clouds
embedded in a stratified gas atmosphere. The resulting differences in sola
r broadband radiative fluxes appear to be neglectable. Thus, a stratified g
aseous atmosphere seems sufficiently adequate for solar radiative transfer
calculations. The reasons for these small differences are basically due to
the strong correlation between cloud optical thickness and water vapour den
sity as produced by the cloud model used in this study. (C) 2000 Elsevier S
cience Ltd. All rights reserved.