Articles | Volume 14, issue 11
https://doi.org/10.5194/tc-14-4083-2020
https://doi.org/10.5194/tc-14-4083-2020
Research article
 | 
18 Nov 2020
Research article |  | 18 Nov 2020

Reconciling the surface temperature–surface mass balance relationship in models and ice cores in Antarctica over the last 2 centuries

Marie G. P. Cavitte, Quentin Dalaiden, Hugues Goosse, Jan T. M. Lenaerts, and Elizabeth R. Thomas

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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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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (09 Sep 2020) by Ruth Mottram
AR by Marie G. P. Cavitte on behalf of the Authors (09 Sep 2020)  Author's response    Manuscript
ED: Publish subject to technical corrections (08 Oct 2020) by Ruth Mottram
AR by Marie G. P. Cavitte on behalf of the Authors (12 Oct 2020)  Author's response    Manuscript
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Short summary
Surface mass balance (SMB) and surface air temperature (SAT) are correlated at the regional scale for most of Antarctica, SMB and δ18O. Areas with low/no correlation are where wind processes (foehn, katabatic wind warming, and erosion) are sufficiently active to overwhelm the synoptic-scale snow accumulation. Measured in ice cores, the link between SMB, SAT, and δ18O is much weaker. Random noise can be removed by core record averaging but local processes perturb the correlation systematically.