Articles | Volume 17, issue 11
https://doi.org/10.5194/tc-17-4779-2023
https://doi.org/10.5194/tc-17-4779-2023
Research article
 | 
10 Nov 2023
Research article |  | 10 Nov 2023

Investigating the spatial representativeness of East Antarctic ice cores: a comparison of ice core and radar-derived surface mass balance over coastal ice rises and Dome Fuji

Marie G. P. Cavitte, Hugues Goosse, Kenichi Matsuoka, Sarah Wauthy, Vikram Goel, Rahul Dey, Bhanu Pratap, Brice Van Liefferinge, Thamban Meloth, and Jean-Louis Tison

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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-2023-65', Steven Franke, 01 Jul 2023
    • AC1: 'Reply on RC1', Marie G. P. Cavitte, 09 Aug 2023
  • RC2: 'Comment on tc-2023-65', Anonymous Referee #2, 09 Jul 2023
    • AC2: 'Reply on RC2', Marie G. P. Cavitte, 09 Aug 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (24 Aug 2023) by Joel Savarino
AR by Marie G. P. Cavitte on behalf of the Authors (04 Sep 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (18 Sep 2023) by Joel Savarino
AR by Marie G. P. Cavitte on behalf of the Authors (25 Sep 2023)
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Short summary
The net accumulation of snow over Antarctica is key for assessing current and future sea-level rise. Ice cores record a noisy snowfall signal to verify model simulations. We find that ice core net snowfall is biased to lower values for ice rises and the Dome Fuji site (Antarctica), while the relative uncertainty in measuring snowfall increases rapidly with distance away from the ice core sites at the ice rises but not at Dome Fuji. Spatial variation in snowfall must therefore be considered.