Cloud condensation nuclei (CCN) are linked to radiative forcing, precipitat
ion, and cloud structure; yet, their role in tropical climates remains larg
ely unknown. CCN concentrations (N-CCN) measured during the wet season in t
he Amazon Basin were surprisingly low (mean N-CCN at 1% supersaturation: 26
7 +/- 132 cm(-3)) and resembled concentrations more typical of marine locat
ions than most continental sites. At low background CCN concentrations, clo
ud properties are more sensitive to an increase in N-CCN. Therefore: enhanc
ed aerosol emissions due to human activity in the Amazon Basin may have a s
tronger impact on climate than emissions in other continental regions. In s
pite of the large organic fraction in the Amazonian aerosol, a detailed ana
lysis of number distributions and size-dependent chemical composition indic
ates that sulfate plays an important role in CCN activity.