Articles | Volume 16, issue 8
https://doi.org/10.5194/tc-16-3033-2022
https://doi.org/10.5194/tc-16-3033-2022
Research article
 | 
01 Aug 2022
Research article |  | 01 Aug 2022

GBaTSv2: a revised synthesis of the likely basal thermal state of the Greenland Ice Sheet

Joseph A. MacGregor, Winnie Chu, William T. Colgan, Mark A. Fahnestock, Denis Felikson, Nanna B. Karlsson, Sophie M. J. Nowicki, and Michael Studinger

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Review of MacGregor et al “GBaTSv2: A revised synthesis of the likely basal thermal state of the Greenland Ice Sheet“', Andy Aschwanden, 29 Apr 2022
  • RC2: 'Comment on tc-2022-40', Anonymous Referee #2, 29 Apr 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (16 Jun 2022) by Alexander Robinson
AR by Joseph MacGregor on behalf of the Authors (22 Jun 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (07 Jul 2022) by Alexander Robinson
AR by Joseph MacGregor on behalf of the Authors (07 Jul 2022)
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Short summary
Where the bottom of the Greenland Ice Sheet is frozen and where it is thawed is not well known, yet knowing this state is increasingly important to interpret modern changes in ice flow there. We produced a second synthesis of knowledge of the basal thermal state of the ice sheet using airborne and satellite observations and numerical models. About one-third of the ice sheet’s bed is likely thawed; two-fifths is likely frozen; and the remainder is too uncertain to specify.