Articles | Volume 18, issue 22
https://doi.org/10.5194/gmd-18-9167-2025
https://doi.org/10.5194/gmd-18-9167-2025
Methods for assessment of models
 | 
27 Nov 2025
Methods for assessment of models |  | 27 Nov 2025

Quantifying coupling errors in atmosphere-ocean-sea ice models: A study of iterative and non-iterative approaches in the EC-Earth AOSCM

Valentina Schüller, Florian Lemarié, Philipp Birken, and Eric Blayo

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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 egusphere-2025-1342', Charles Pelletier, 09 Jul 2025
    • AC1: 'Clarification Questions on RC1', Valentina Schüller, 14 Jul 2025
      • RC2: 'Reply on AC1', Charles Pelletier, 14 Jul 2025
        • AC3: 'Reply on RC2', Valentina Schüller, 10 Sep 2025
  • RC3: 'Comment on egusphere-2025-1342', Anonymous Referee #2, 08 Aug 2025
    • AC4: 'Reply on RC3', Valentina Schüller, 10 Sep 2025
  • AC2: 'Comment on egusphere-2025-1342', Valentina Schüller, 10 Sep 2025

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Valentina Schüller on behalf of the Authors (10 Sep 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (11 Sep 2025) by Qiang Wang
RR by Charles Pelletier (15 Sep 2025)
RR by Anonymous Referee #2 (13 Oct 2025)
ED: Publish subject to minor revisions (review by editor) (20 Oct 2025) by Qiang Wang
AR by Valentina Schüller on behalf of the Authors (23 Oct 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (05 Nov 2025) by Qiang Wang
AR by Valentina Schüller on behalf of the Authors (07 Nov 2025)
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Short summary
Earth system models consist of many components, coupled in time and space. Standard coupling algorithms introduce a numerical error, which one can compute with iterative coupling methods. We use such a method for a coupled model of a single vertical column of the atmosphere, ocean, and sea ice. We find that coupling errors in the atmosphere and at the ice surface can be substantial and that discontinuous physics parameterizations lead to convergence issues of the iteration.
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