Articles | Volume 15, issue 23
https://doi.org/10.5194/acp-15-13339-2015
https://doi.org/10.5194/acp-15-13339-2015
Research article
 | 
02 Dec 2015
Research article |  | 02 Dec 2015

Boundary layer new particle formation over East Antarctic sea ice – possible Hg-driven nucleation?

R. S. Humphries, R. Schofield, M. D. Keywood, J. Ward, J. R. Pierce, C. M. Gionfriddo, M. T. Tate, D. P. Krabbenhoft, I. E. Galbally, S. B. Molloy, A. R. Klekociuk, P. V. Johnston, K. Kreher, A. J. Thomas, A. D. Robinson, N. R. P. Harris, R. Johnson, and S. R. Wilson

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Ruhi Humphries on behalf of the Authors (07 Oct 2015)
ED: Referee Nomination & Report Request started (28 Oct 2015) by Peter DeCarlo
RR by Anonymous Referee #2 (11 Nov 2015)
ED: Publish subject to technical corrections (11 Nov 2015) by Peter DeCarlo
AR by Ruhi Humphries on behalf of the Authors (18 Nov 2015)  Author's response   Manuscript 
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Short summary
An atmospheric new particle formation event that was observed in the pristine East Antarctic pack ice during a springtime voyage in 2012 is characterised in terms of formation and growth rates. Known nucleation mechanisms (e.g. those involving sulfate, iodine and organics) were unable to explain observations; however, correlations with total gaseous mercury were found, leading to the suggestion of a possible mercury-driven nucleation mechanism not previously described.
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