Articles | Volume 17, issue 5
https://doi.org/10.5194/os-17-1177-2021
https://doi.org/10.5194/os-17-1177-2021
Research article
 | 
02 Sep 2021
Research article |  | 02 Sep 2021

Regional imprints of changes in the Atlantic Meridional Overturning Circulation in the eddy-rich ocean model VIKING20X

Arne Biastoch, Franziska U. Schwarzkopf, Klaus Getzlaff, Siren Rühs, Torge Martin, Markus Scheinert, Tobias Schulzki, Patricia Handmann, Rebecca Hummels, and Claus W. Böning

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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 os-2021-37', Anonymous Referee #1, 22 Jun 2021
    • AC1: 'Reply on RC1', Arne Biastoch, 19 Jul 2021
  • RC2: 'Comment on os-2021-37', Anonymous Referee #2, 08 Jul 2021
    • AC2: 'Reply on RC2', Arne Biastoch, 19 Jul 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Arne Biastoch on behalf of the Authors (19 Jul 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (03 Aug 2021) by Matthew Hecht
AR by Franziska Schwarzkopf on behalf of the Authors (04 Aug 2021)  Manuscript 
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Short summary
The Atlantic Meridional Overturning Circulation (AMOC) quantifies the impact of the ocean on climate and climate change. Here we show that a high-resolution ocean model is able to realistically simulate ocean currents. While the mean representation of the AMOC depends on choices made for the model and on the atmospheric forcing, the temporal variability is quite robust. Comparing the ocean model with ocean observations, we able to identify that the AMOC has declined over the past two decades.