Solid organic-coated ammonium sulfate particles at high relative humidity in the summertime Arctic atmosphere

• Published in: Proceedings of the National Academy of Sciences
• Main Authors: Kirpes, Rachel, Lei, Ziying, Fraund, Matthew, Gunsch, Matthew J., May, Nathaniel W., Barrett, Tate E., Moffett, Claire E., Schauer, Andrew, Alexander, Becky, Upchurch, Lucia, China, Swarup, Quinn, Patricia K., Moffet, Ryan, Laskin, Alexander, Sheesley, Rebecca J., Pratt, Kerri A., Ault, Andrew P.
• Language: unknown
• Published: 2022
• Subjects: 54 ENVIRONMENTAL SCIENCES; Aitken; Arctic; Arctic Ocean; Sea ice
• Online Access: http://www.osti.gov/servlets/purl/1862855; https://www.osti.gov/biblio/1862855; https://doi.org/10.1073/pnas.2104496119

The ability of atmospheric aerosols to impact climate through water uptake and cloud formation is fundamentally determined by the size, composition, and phase (liquid, semisolid, or solid) of individual particles. Particle phase is dependent on atmospheric conditions (relative humidity and temperature) and chemical composition and, importantly, solid particles can inhibit the uptake of water and other trace gases, even under humid conditions. Particles composed primarily of ammonium sulfate are presumed to be liquid at the relative humidities (67 to 98%) and temperatures (–2 to 4 °C) of the summertime Arctic. Under these atmospheric conditions, we report the observation of solid organic-coated ammonium sulfate particles representing 30% of particles, by number, in a key size range (<0.2 µm) for cloud activation within marine air masses from the Arctic Ocean at Utqiagvik, AK. The composition and size of the observed particles are consistent with recent Arctic modeling and observational results showing new particle formation and growth from dimethylsulfide oxidation to form sulfuric acid, reaction with ammonia, and condensation of marine biogenic sulfate and highly oxygenated organic molecules. Aqueous sulfate particles typically undergo efflorescence and solidify at relative humidities of less than 34%. Therefore, the observed solid phase is hypothesized to occur from contact efflorescence during collision of a newly formed Aitken mode sulfate particle with an organic-coated ammonium sulfate particle. With declining sea ice in the warming Arctic, this particle source is expected to increase with increasing open water and marine biogenic emissions.