Articles | Volume 17, issue 4
https://doi.org/10.5194/cp-17-1685-2021
https://doi.org/10.5194/cp-17-1685-2021
Research article
 | 
11 Aug 2021
Research article |  | 11 Aug 2021

Applying an isotope-enabled regional climate model over the Greenland ice sheet: effect of spatial resolution on model bias

Marcus Breil, Emanuel Christner, Alexandre Cauquoin, Martin Werner, Melanie Karremann, and Gerd Schädler

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Interactive discussion

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 (07 Sep 2020) by André Paul
AR by Marcus Breil on behalf of the Authors (12 Oct 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (20 Oct 2020) by André Paul
RR by Anonymous Referee #2 (17 Jan 2021)
ED: Reconsider after major revisions (01 Feb 2021) by André Paul
AR by Marcus Breil on behalf of the Authors (29 Mar 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (26 May 2021) by André Paul
RR by Anonymous Referee #2 (02 Jul 2021)
ED: Publish subject to technical corrections (10 Jul 2021) by André Paul
AR by Marcus Breil on behalf of the Authors (13 Jul 2021)  Manuscript 
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Short summary
For the first time an isotope-enabled regional climate simulation for Greenland is performed for the mid-Holocene. Simulation results are compared with observed isotope ratios in ice cores. Compared to global climate simulations, a regional downscaling improves the agreement with measured isotope concentrations. Thus, an isotope-enabled regional climate simulation constitutes a useful supplement to reconstruct regional paleo-climate conditions during the mid-Holocene in Greenland.