Articles | Volume 18, issue 18
https://doi.org/10.5194/gmd-18-6313-2025
https://doi.org/10.5194/gmd-18-6313-2025
Methods for assessment of models
 | 
25 Sep 2025
Methods for assessment of models |  | 25 Sep 2025

Constraining CMIP6 sea ice simulations with ICESat-2

Alek Petty, Christopher Cardinale, and Madison Smith

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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-2025-766', Anonymous Referee #1, 12 Apr 2025
  • RC2: 'Comment on egusphere-2025-766', Anonymous Referee #2, 15 Apr 2025
  • AC3: 'Comment on egusphere-2025-766', Alek Petty, 02 May 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Alek Petty on behalf of the Authors (20 May 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (10 Jun 2025) by Christopher Horvat
AR by Alek Petty on behalf of the Authors (13 Jun 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (18 Jun 2025) by Christopher Horvat
AR by Alek Petty on behalf of the Authors (27 Jun 2025)
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Short summary
We use total freeboard data from NASA’s Ice, Cloud and land Elevation Satellite-2 (ICESat-2) across both hemispheres and estimates of winter Arctic sea ice thickness to evaluate climate model simulations of sea ice, providing constraints beyond the traditional sea ice area metric. ICESat-2 provides accurate freeboard data, but its short observational record requires careful consideration of natural variability.
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