Impact of Aerosol-Cloud Cycling on Aqueous Secondary Organic Aerosol Formation

• Published in: Atmosphere Vol. 10; no. 11; p. 666
• Main Authors: Tsui, William G., Woo, Joseph L., McNeill, V. Faye
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01-11-2019
• Subjects: Aerosol effects; Aerosol formation; Aerosol particles; Aerosols; aqueous aerosol; Atmospheric aerosols; Atmospheric chemistry; Atmospheric models; Chemical reactions; Clouds; cloudwater; Cycles; Humidity; Isoprene; isoprene epoxydiol; Laboratories; Mass transfer; Moisture content; Morphology; Organic acids; Organic coatings; pH effects; Photochemicals; Photochemistry; Secondary aerosols; secondary organic aerosol; Simulation; Time of use; Uptake; Viscosity; Water content; Whiteface Mountain
• ISSN: 2073-4433; 2073-4433
• DOI: 10.3390/atmos10110666

Chemical processing of organic material in aqueous atmospheric aerosols and cloudwater is known to form secondary organic aerosols (SOA), although the extent to which each of these processes contributes to total aerosol mass is unclear. In this study, we use GAMMA 5.0, a photochemical box model with coupled gas and aqueous-phase chemistry, to consider the impact of aqueous organic reactions in both aqueous aerosols and clouds on isoprene epoxydiol (IEPOX) SOA over a range of pH for both aqueous phases, including cycling between cloud and aerosol within a single simulation. Low pH aqueous aerosol, in the absence of organic coatings or other morphology which may limit uptake of IEPOX, is found to be an efficient source of IEPOX SOA, consistent with previous work. Cloudwater at pH 4 or lower is also found to be a potentially significant source of IEPOX SOA. This phenomenon is primarily attributed to the relatively high uptake of IEPOX to clouds as a result of higher water content in clouds as compared with aerosol. For more acidic cloudwater, the aqueous organic material is comprised primarily of IEPOX SOA and lower-volatility organic acids. Both cloudwater pH and the time of day or sequence of aerosol-to-cloud or cloud-to-aerosol transitions impacted final aqueous SOA mass and composition in the simulations. The potential significance of cloud processing as a contributor to IEPOX SOA production could account for discrepancies between predicted IEPOX SOA mass from atmospheric models and measured ambient IEPOX SOA mass, or observations of IEPOX SOA in locations where mass transfer limitations are expected in aerosol particles.