The unique Khrgian-Mazin size distribution is suggested as an alternat
ive approximation of the entire drop spectra besides the conventional
approximation in which the monodisperse and the Marshall-Palmer size d
istributions for cloud droplets and raindrops are used, respectively.
This approach is employed in bulk microphysics. It is shown that the e
ffects of the changed drop size distribution are particularly pronounc
ed in the case of the microphysical production terms with rain. This i
s a consequence of the fact that the Khrgian-Mazin size distribution p
roduces more small raindrops and less large ones compared to the Marsh
all-Palmer one, where both have the same rain water mixing ratio. The
new production terms with cloud water do not differ from those with th
e monodisperse size distribution used. In order to show the sensitivit
y of cloud microphysics with respect to the change of drop size distri
bution function, the experiments are perform with the two versions of
a forced 1-D time-dependent model. The first one involves the microphy
sical production terms with the Khrgian-Mazin size distribution, while
the other one uses the conventional approach. Experiments clearly sho
w that cloud microphysics essentially depends on cloud drop size distr
ibution. Some microphysical aspects of a model cloud with the new drop
size distribution are in fair agreement with observations. (C) 1998 E
lsevier Science B.V. All rights reserved.