A numerical model for a drop convective cloud with detailed microphysics, c
hemistry, and radiation is presented. The condensation and coagulation proc
esses are described with the help of a kinetic equation. The coagulation is
calculated using a modification of the well-known Kowetz-Alund method. The
chemical model includes about 150 gas-phase reactions (with a detailed des
cription of transformations in the oxygen, nitrogen, hydrogen, chlorine, su
lfur, methane, and ethane cycles) and about 110 aqueous-phase reactions (in
cluding both the interphase and aqueous-phase steady-state reactions) that
account for diffusion and gas absorption on the cloud drop surfaces. The ph
otodissociation rates in the radiative transfer module are calculated using
the delta-Eddington scheme. The results of numerical experiments indicate
that convective clouds in the troposphere tend to decrease the concentratio
ns of highly soluble species due to their capture by the cloud drops and fu
rther precipitation scavenging. The vertical transport in convective clouds
significantly affects the concentrations of slightly soluble gases. The ra
diative processes in clouds have a profound impact on the concentrations of
short-lived gaseous species. It is also shown that the aqueous-phase chemi
stry calculations must include not only the chemical reactions but also the
species redistribution over drop sizes during condensation-evaporation and
coagulation processes.