Summertime Primary and Secondary Contributions to Southern Ocean Cloud Condensation Nuclei

• Published in: Scientific Reports
• Main Authors: Fossum, Kirsten N., Dall'Osto, Manuel, Simó, Rafel, O'Dowd, Colin D.
• Other Authors: Natural Sciences and Engineering Research Council of Canada, Centre National D'Etudes Spatiales (France), European Commission, Ministerio de Economía y Competitividad (España)
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Springer Nature 2018
• Subjects: Antarctic; Mace; Southern Ocean; Antarc*; Antarctica
• Online Access: http://hdl.handle.net/10261/172692; https://doi.org/10.1038/s41598-018-32047-4; https://doi.org/10.13039/501100000038; https://doi.org/10.13039/501100002830; https://doi.org/10.13039/501100000780; https://doi.org/10.13039/501100003329

14 pages, 2 figures, 3 tables, supplementary information https://dx.doi.org/10.1038/s41598-018-32047-4.-- Author correction Scientific Reports 9: 10613 (2019), https://dx.doi.org/10.1038/s41598-019-46788-3 Atmospheric aerosols in clean remote oceanic regions contribute significantly to the global albedo through the formation of haze and cloud layers; however, the relative importance of ‘primary’ wind-produced sea-spray over secondary (gas-to-particle conversion) sulphate in forming marine clouds remains unclear. Here we report on marine aerosols (PM) over the Southern Ocean around Antarctica, in terms of their physical, chemical, and cloud droplet activation properties. Two predominant pristine air masses and aerosol populations were encountered: modified continental Antarctic (cAA) comprising predominantly sulphate with minimal sea-salt contribution and maritime Polar (mP) comprising sulphate plus sea-salt. We estimate that in cAA air, 75% of the CCN are activated into cloud droplets while in mP air, 37% are activated into droplets, for corresponding peak supersaturation ranges of 0.37–0.45% and 0.19–0.31%, respectively. When realistic marine boundary layer cloud supersaturations are considered (e.g. ~0.2–0.3%), sea-salt CCN contributed 2–13% of the activated nuclei in the cAA air and 8–51% for the marine air for surface-level wind speed < 16 m s. At higher wind speeds, primary marine aerosol can even contribute up to 100% of the activated CCN, for corresponding peak supersaturations as high as 0.32% The research leading to these results has received funding from the European Union’s Seventh Framework Programme (FP7/2007-2013) project BACCHUS under grant agreement n_ 603445; Spanish Ministry of Economy and Competitiveness (MINECO) as part of the PEGASO (Ref.: CTM2012-37615) and BIO-NUC (Ref: CGL2013-49020-R) projects; HEA-PRTLI4 and SFI under MaREI. EPA Ireland is acknowledged for research support at Mace Head. M.B. received funding through the Italian RITMARE fellowship and is now funded by the postdoc ...