Significance Organic aerosol (OA) is a dominant component of atmospheric aerosol worldwide, and it is recognized as a key factor affecting air quality and possibly climate. Observations indicate that more than one-half of the global OA is of secondary origin. Traditional models typically underpredict secondary organic aerosol (SOA) mass, suggesting that a complete knowledge of SOA formation mechanisms is lacking. We show that aqueous-phase processing of biomass-burning emissions contributes to SOA formation. Such aqueous SOA absorbs UV and visible light more efficiently that other OA components. Aqueous chemistry processing of biomass-burning emissions should be taken into account in air quality and climate models for a correct description of the global OA budget and its climate-relevant optical properties.