Smoke particles from biomass burning can generate forcing of climate b
y modifying cloud microphysics and reflectance of sunlight. Cloud modi
fication, critical to an understanding of climate change, is uncertain
and variable. Satellite data over the Amazon Basin and Cerrado were a
nalyzed for cloud reflectance and droplet size and for smoke concentra
tion. Smoke increased cloud reflectance from 0.35 to 0.35, while reduc
ing droplet size from 14 to 9 micrometers. The regional variability of
the smoke effect was correlated to the availability of water vapor. D
uring the 3 months of biomass burning in the dry season, the smoke-clo
ud forcing of climate was only -2 watts per square meter in this regio
n, much smaller than what can be inferred from model predictions.