Articles | Volume 14, issue 11
https://doi.org/10.5194/tc-14-4181-2020
https://doi.org/10.5194/tc-14-4181-2020
Research article
 | 
25 Nov 2020
Research article |  | 25 Nov 2020

Long-term surface energy balance of the western Greenland Ice Sheet and the role of large-scale circulation variability

Baojuan Huai, Michiel R. van den Broeke, and Carleen H. Reijmer

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (13 Aug 2020) by Valentina Radic
AR by Huai baojuan on behalf of the Authors (14 Aug 2020)  Author's response 
ED: Referee Nomination & Report Request started (30 Aug 2020) by Valentina Radic
RR by Federico Covi (15 Sep 2020)
ED: Publish subject to revisions (further review by editor and referees) (04 Oct 2020) by Valentina Radic
AR by Huai baojuan on behalf of the Authors (09 Oct 2020)  Author's response   Manuscript 
ED: Publish as is (11 Oct 2020) by Valentina Radic
AR by Huai baojuan on behalf of the Authors (20 Oct 2020)
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Short summary
This study presents the surface energy balance (SEB) of the Greenland Ice Sheet (GrIS) using a SEB model forced with observations from automatic weather stations (AWSs). We correlate ERA5 with AWSs to show a significant positive correlation of GrIS summer surface temperature and melt with the Greenland Blocking Index and weaker and opposite correlations with the North Atlantic Oscillation. This analysis may help explain melting patterns in the GrIS with respect to circulation anomalies.