Articles | Volume 16, issue 8
https://doi.org/10.5194/tc-16-3375-2022
https://doi.org/10.5194/tc-16-3375-2022
Research article
 | Highlight paper
 | 
29 Aug 2022
Research article | Highlight paper |  | 29 Aug 2022

The impact of climate oscillations on the surface energy budget over the Greenland Ice Sheet in a changing climate

Tiago Silva, Jakob Abermann, Brice Noël, Sonika Shahi, Willem Jan van de Berg, and Wolfgang Schöner

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on tc-2021-388', Anonymous Referee #1, 01 Feb 2022
    • AC1: 'Reply on RC1', Tiago Silva, 15 Apr 2022
  • RC2: 'Comment on tc-2021-388', Anonymous Referee #2, 01 Feb 2022
    • AC2: 'Reply on RC2', Tiago Silva, 15 Apr 2022
  • RC3: 'Comment on tc-2021-388', Anonymous Referee #3, 11 Feb 2022
    • AC3: 'Reply on RC3', Tiago Silva, 15 Apr 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (22 Apr 2022) by Xavier Fettweis
AR by Tiago Silva on behalf of the Authors (15 Jun 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (05 Jul 2022) by Xavier Fettweis
RR by Anonymous Referee #2 (11 Jul 2022)
RR by Anonymous Referee #1 (12 Jul 2022)
RR by Anonymous Referee #3 (14 Jul 2022)
ED: Publish subject to minor revisions (review by editor) (19 Jul 2022) by Xavier Fettweis
AR by Tiago Silva on behalf of the Authors (28 Jul 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (29 Jul 2022) by Xavier Fettweis
AR by Tiago Silva on behalf of the Authors (03 Aug 2022)  Manuscript 
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Co-editor-in-chief
This paper shows that the changes observed in the North of the Greenland ice sheet mainly result from Arctic sea ice decline and are less dependent on the atmospheric circulation variability in North-Atlantic sector. The sea ice decline, therefore, exerts another (indirect) anthropogenic-driven influence on mass loss in Greenland.
Short summary
To overcome internal climate variability, this study uses k-means clustering to combine NAO, GBI and IWV over the Greenland Ice Sheet (GrIS) and names the approach as the North Atlantic influence on Greenland (NAG). With the support of a polar-adapted RCM, spatio-temporal changes on SEB components within NAG phases are investigated. We report atmospheric warming and moistening across all NAG phases as well as large-scale and regional-scale contributions to GrIS mass loss and their interactions.