Articles | Volume 20, issue 9
https://doi.org/10.5194/cp-20-2001-2024
https://doi.org/10.5194/cp-20-2001-2024
Research article
 | 
12 Sep 2024
Research article |  | 12 Sep 2024

Glacial AMOC shoaling despite vigorous tidal dissipation: vertical stratification matters

Yugeng Chen, Pengyang Song, Xianyao Chen, and Gerrit Lohmann

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (19 Jun 2024) by Marisa Montoya
AR by Yugeng Chen on behalf of the Authors (27 Jun 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (04 Jul 2024) by Marisa Montoya
RR by Anonymous Referee #1 (08 Jul 2024)
RR by Guido Vettoretti (19 Jul 2024)
ED: Publish subject to technical corrections (23 Jul 2024) by Marisa Montoya
AR by Yugeng Chen on behalf of the Authors (23 Jul 2024)  Manuscript 
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Short summary

Our study examines the Atlantic Meridional Overturning Circulation (AMOC) during the Last Glacial Maximum (LGM), a period with higher tidal dissipation. Despite increased tidal mixing, our model simulations show that the AMOC remained relatively shallow, consistent with paleoproxy data and resolving previous inconsistencies between proxy data and model simulations. This research highlights the importance of strong ocean stratification during the LGM and its interaction with tidal mixing.