compounds (BVOCs), contribute large uncertainties to the radiative forcing that is associated
with aerosols in the climate system. Reactive uptake of surface-active organic oxidation
products of BVOCs at the gas–aerosol interface can potentially decrease the overall aerosol
surface tension and therefore influence their propensity to act as cloud condensation nuclei
(CCN). Here, we synthesize and measure some climate-relevant physical properties of SOA …