Articles | Volume 19, issue 11
Atmos. Chem. Phys., 19, 7467–7485, 2019
https://doi.org/10.5194/acp-19-7467-2019
Atmos. Chem. Phys., 19, 7467–7485, 2019
https://doi.org/10.5194/acp-19-7467-2019

Research article 05 Jun 2019

Research article | 05 Jun 2019

Supercooled liquid fogs over the central Greenland Ice Sheet

Christopher J. Cox et al.

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 Lorena Grabowski on behalf of the Authors (26 Feb 2019)  Author's response
ED: Referee Nomination & Report Request started (06 Mar 2019) by Martina Krämer
RR by Anonymous Referee #1 (27 Mar 2019)
ED: Reconsider after major revisions (08 Apr 2019) by Martina Krämer
AR by Svenja Lange on behalf of the Authors (15 Apr 2019)  Author's response
ED: Referee Nomination & Report Request started (24 Apr 2019) by Martina Krämer
RR by Anonymous Referee #1 (05 May 2019)
ED: Publish subject to technical corrections (07 May 2019) by Martina Krämer
AR by Christopher Cox on behalf of the Authors (22 May 2019)  Author's response    Manuscript
Download
Short summary
Fogs are frequently reported by observers on the Greenland Ice Sheet. Fogs play a role in the hydrological and energetic balances of the ice sheet surface, but as yet the properties of Greenland fogs are not well known. We observed fogs in all months from Summit Station for 2 years and report their properties. Annually, fogs impart a slight warming to the surface and a case study suggests that they are particularly influential by providing insulation during the coldest part of the day in summer.
Altmetrics
Final-revised paper
Preprint