A parameterization of cloud droplet nucleation for a single, log-norma
lly distributed, aerosol type is generalized to the case of multiple a
erosol types with differing size distributions and compositions. The p
arameterization accounts for the competition between different aerosol
types as cloud condensation nuclei, and the dependence of the competi
tion on the number concentration, composition and size distribution of
each aerosol type. Comparisons with detailed numerical solutions indi
cate typical differences of 50% and 20% for the number fraction and ma
ss fraction, respectively of aerosols activated for each type.