Articles | Volume 21, issue 3
https://doi.org/10.5194/os-21-1081-2025
https://doi.org/10.5194/os-21-1081-2025
Research article
 | 
20 Jun 2025
Research article |  | 20 Jun 2025

Stratification and overturning circulation are intertwined controls on ocean heat uptake efficiency in climate models

Linus Vogt, Jean-Baptiste Sallée, and Casimir de Lavergne

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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-2024-3442', Anonymous Referee #1, 29 Dec 2024
    • AC2: 'Reply on RC1', Linus Vogt, 19 Mar 2025
  • RC2: 'Comment on egusphere-2024-3442', Timothée Bourgeois, 29 Jan 2025
    • AC1: 'Reply on RC2', Linus Vogt, 19 Mar 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Linus Vogt on behalf of the Authors (19 Mar 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (25 Mar 2025) by Katsuro Katsumata
AR by Linus Vogt on behalf of the Authors (26 Mar 2025)  Manuscript 
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Short summary
The ocean buffers human-induced climate change by taking up excess heat from the atmosphere. In this study, we use an ensemble of global climate models to study the physical processes which set the efficiency at which this heat is stored in the ocean. We reconcile previous attempts to explain controls on this efficiency and find that Southern Ocean stratification is a key model property due to its influence on the local overturning circulation and its connection to the subpolar North Atlantic.
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