Articles | Volume 13, issue 1
Earth Syst. Dynam., 13, 303–319, 2022
https://doi.org/10.5194/esd-13-303-2022
Earth Syst. Dynam., 13, 303–319, 2022
https://doi.org/10.5194/esd-13-303-2022

Research article 02 Feb 2022

Research article | 02 Feb 2022

Climate change signal in the ocean circulation of the Tyrrhenian Sea

Alba de la Vara et al.

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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 esd-2021-37', Anonymous Referee #1, 01 Jul 2021
  • RC2: 'Comment on esd-2021-37', Anonymous Referee #2, 03 Jul 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (07 Sep 2021) by Yun Liu
AR by Alba de la Vara on behalf of the Authors (15 Sep 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (26 Sep 2021) by Yun Liu
RR by Anonymous Referee #1 (09 Oct 2021)
RR by Anonymous Referee #2 (12 Oct 2021)
ED: Publish subject to minor revisions (review by editor) (29 Oct 2021) by Yun Liu
AR by Alba de la Vara on behalf of the Authors (15 Nov 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (02 Dec 2021) by Yun Liu
AR by Alba de la Vara on behalf of the Authors (09 Dec 2021)  Author's response    Manuscript
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Short summary
We study with the regionally coupled climate model ROM the impact of climate change on the Tyrrhenian Sea circulation, as well as the possible mechanisms and consequences in the NW Mediterranean Sea. Our results show a shift towards the summer circulation pattern by the end of the century. Also, water flowing via the Corsica Channel is more stratified and smaller in volume. Both factors may contribute to the interruption of deep water formation in the Gulf of Lions in the future.
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