Articles | Volume 19, issue 8
https://doi.org/10.5194/acp-19-5737-2019
https://doi.org/10.5194/acp-19-5737-2019
Research article
 | 
30 Apr 2019
Research article |  | 30 Apr 2019

Investigation of coastal sea-fog formation using the WIBS (wideband integrated bioaerosol sensor) technique

Shane M. Daly, David J. O'Connor, David A. Healy, Stig Hellebust, Jovanna Arndt, Eoin J. McGillicuddy, Patrick Feeney, Michael Quirke, John C. Wenger, and John R. Sodeau

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by John Sodeau on behalf of the Authors (10 Dec 2018)
ED: Referee Nomination & Report Request started (11 Jan 2019) by Gordon McFiggans
RR by Anonymous Referee #1 (18 Jan 2019)
RR by Anonymous Referee #2 (25 Jan 2019)
ED: Publish subject to minor revisions (review by editor) (03 Mar 2019) by Gordon McFiggans
AR by John Sodeau on behalf of the Authors (12 Mar 2019)  Author's response   Manuscript 
ED: Publish as is (13 Mar 2019) by Gordon McFiggans
AR by John Sodeau on behalf of the Authors (30 Mar 2019)  Manuscript 
Download
Short summary
For a long time sea-salt particles were considered the only types of particles that drive sea-fog formation but recently iodine oxide particles released from kelp have been identified as a source. There are no previous field studies to provide a direct timeline link between molecular iodine release, particle formation and sea-fog formation. The present observations from Cork Harbour provide such a link. A stabilizing mechanism enhancing distribution of iodine in the troposphere is suggested.
Altmetrics
Final-revised paper
Preprint