Microphysical measurements performed during 8 flights of the CLOUDYCOLUMN c
omponent of ACE-2, with the Meteo-France Merlin-IV, are analyzed in terms o
f droplet number concentration and size. The droplet concentration is depen
dent upon the aerosol properties within the boundary layer. Its mean value
over a flight varies from 55 cm(-3), for the cleanest conditions, to 244 cm
(-3), for the most polluted one. For each flight, the variability of the co
ncentration, in selected cloud regions that are not affected by mixing with
dry air or drizzle scavenging, ranges from 0.5 to 1.5 of the mean value. T
he mean volume diameter increases with altitude above cloud base according
to the adiabatic cloud model. The frequency distribution of mean droplet vo
lume normalized by the adiabatic value, for the selected regions, shows the
same dispersion as the distribution of normalized concentration. The value
s of droplet concentration versus mean volume diameter are then examined in
sub-adiabatic samples to characterize the effects of mixing and drizzle sc
avenging. Finally, the ratio of mean volume diameter to effective diameter
is analyzed and a simple relationship between these 2 crucial parameters is
proposed.