Articles | Volume 19, issue 11
https://doi.org/10.5194/acp-19-7467-2019
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, David C. Noone, Max Berkelhammer, Matthew D. Shupe, William D. Neff, Nathaniel B. Miller, Von P. Walden, and Konrad Steffen

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 Christopher Cox on behalf of the Authors (18 Feb 2019)
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 Christopher Cox on behalf of the Authors (11 Apr 2019)
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