Articles | Volume 21, issue 6
https://doi.org/10.5194/os-21-2895-2025
https://doi.org/10.5194/os-21-2895-2025
Research article
 | 
13 Nov 2025
Research article |  | 13 Nov 2025

Diagnosing the Atlantic Meridional Overturning Circulation in density space is critical in warmer climates

Fernanda DI Alzira Oliveira Matos, Dmitry Sidorenko, Xiaoxu Shi, Lars Ackermann, Janini Pereira, Gerrit Lohmann, and Christian Stepanek

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-2326', Anonymous Referee #1, 26 Jun 2025
  • RC2: 'Comment on egusphere-2025-2326', Henri Drake, 25 Jul 2025
  • EC1: 'Comment on egusphere-2025-2326', Julian Mak, 25 Jul 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Fernanda DI Alzira Oliveira Matos on behalf of the Authors (19 Aug 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (19 Aug 2025) by Julian Mak
RR by Henri Drake (16 Sep 2025)
ED: Reconsider after major revisions (17 Sep 2025) by Julian Mak
AR by Fernanda DI Alzira Oliveira Matos on behalf of the Authors (23 Sep 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (24 Sep 2025) by Julian Mak
RR by Henri Drake (13 Oct 2025)
ED: Publish subject to minor revisions (review by editor) (13 Oct 2025) by Julian Mak
AR by Fernanda DI Alzira Oliveira Matos on behalf of the Authors (15 Oct 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (17 Oct 2025) by Julian Mak
AR by Fernanda DI Alzira Oliveira Matos on behalf of the Authors (20 Oct 2025)  Author's response   Manuscript 
Download
Short summary
The Atlantic Meridional Overturning Circulation (AMOC) is responsible for about 25 % of the poleward ocean heat transport. Currently, the AMOC strength is mostly calculated in depth space (z-AMOC). However, we argue that, in warmer climates, the AMOC should be calculated in density space (ρ-AMOC). We performed simulations with CO2 forcing of 280 ppmv (PI) and 1120 ppmv of (4xCO2) and find that ρ-AMOC provides more physical and meaningful information about the AMOC in warmer climates.
Share