Progress has been made over the past decade in predicting secondary organic aerosol
(SOA) mass in the atmosphere using vapor pressure-driven partitioning, which implies that …

Atmospheric aerosol particles serve as condensation nuclei for the formation of both, cloud
droplets and atmospheric ice particles. As a result, they exert a substantial influence on the …

Secondary organic aerosol (SOA) accounts for a significant fraction of ambient tropospheric
aerosol and a detailed knowledge of the formation, properties and transformation of SOA is …

We present a method to describe the relationship between particle dry diameter and cloud
condensation nuclei (CCN) activity using a single hygroscopicity parameter κ. Values of the …

Aerosol− cloud interactions account for the largest uncertainty in current estimates of
changes in radiative forcing according to the most recent IPCC report. 1 The term “aerosol …

Size-resolved cloud condensation nuclei (CCN) spectra measured for various aerosol types
at a non-urban site in Germany showed that CCN concentrations are mainly determined by …

Aerosol forcing uncertainty represents the largest climate forcing uncertainty overall. Its
magnitude has remained virtually undiminished over the past 20 years despite considerable …

The effects of atmospheric aerosol on climate forcing may be very substantial but are
quantified poorly at present; in particular, the effects of aerosols on cloud radiative …

We have investigated the formation of cloud droplets under pyro-convective conditions using
a cloud parcel model with detailed spectral microphysics and with the κ-Köhler model …

Aqueous extracts of secondary organic aerosols (SOA) generated from the ozonolysis of d‐
limonene were subjected to dissolution, evaporation, and re‐dissolution in the presence and …