Articles | Volume 16, issue 8
The Cryosphere, 16, 3033–3049, 2022
https://doi.org/10.5194/tc-16-3033-2022
The Cryosphere, 16, 3033–3049, 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 et al.

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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
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
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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.