Characterizing the hygroscopicity of growing particles in the Canadian Arctic summer

• Published in: Atmospheric Chemistry and Physics
• Main Authors: R. Y.-W. Chang, J. P. D. Abbatt, M. C. Boyer, J. P. Chaubey, D. B. Collins
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: Physics; QC1-999; Chemistry; QD1-999; Arctic; Canadian Arctic Archipelago; Arctic Archipelago
• Online Access: https://doi.org/10.5194/acp-22-8059-2022; https://doaj.org/article/586643ebe56b4802877d35282f4bd7db

The impact of aerosols on clouds is a well-studied, although still poorly constrained, part of the atmospheric system. New particle formation (NPF) is thought to contribute 40 %–80 % of the global cloud droplet number concentration, although it is extremely difficult to observe an air mass from NPF to cloud formation. NPF and growth occurs frequently in the Canadian Arctic summer atmosphere, although only a few studies have characterized the source and properties of these aerosols. This study presents cloud condensation nuclei (CCN) concentrations measured on board the CCGS Amundsen in the eastern Canadian Arctic Archipelago from 23 July to 23 August 2016 as part of the Network on Climate and Aerosols: Addressing Uncertainties in Remote Canadian Environments (NETCARE). The study was dominated by frequent ultrafine particle and/or growth events, and particles smaller than 100 nm dominated the size distribution for 92 % of the study period. Using κ -Köhler theory and aerosol size distributions, the mean hygroscopicity parameter ( κ ) calculated for the entire study was 0.12 (0.06–0.12, 25th–75th percentile), suggesting that the condensable vapours that led to particle growth were primarily slightly hygroscopic, which we infer to be organic. Based on past measurement and modelling studies from NETCARE and the Canadian Arctic, it seems likely that the source of these slightly hygroscopic, organic, vapours is the ocean. Examining specific growth events suggests that the mode diameter ( D max ) had to exceed 40 nm before CCN concentrations at 0.99 % supersaturation (SS) started to increase, although a statistical analysis shows that CCN concentrations increased 13–274 cm −3 during all ultrafine particle and/or growth times (total particle concentrations >500 cm −3 , D max <100 nm) compared with background times (total concentrations <500 cm −3 ) at SS of 0.26 %–0.99 %. This value increased to 25–425 cm −3 if the growth times were limited to times when D max was also larger than 40 nm. These results support ...