Articles | Volume 22, issue 6
https://doi.org/10.5194/os-22-3723-2026
https://doi.org/10.5194/os-22-3723-2026
Research article
 | 
13 Nov 2026
Research article |  | 13 Nov 2026

Recent thermohaline shifts in the Adriatic Sea and their potential consequences

Elena Terzić and Ivica Vilibić

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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-2026-3080', Anonymous Referee #1, 27 Jul 2026
    • AC1: 'Reply on RC1', Ivica Vilibić, 07 Sep 2026
  • RC2: 'Comment on egusphere-2026-3080', Anonymous Referee #2, 11 Aug 2026
    • AC1: 'Reply on RC1', Ivica Vilibić, 07 Sep 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Reconsider after major revisions (11 Sep 2026) by Mario Hoppema
AR by Ivica Vilibić on behalf of the Authors (11 Sep 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (14 Sep 2026) by Mario Hoppema
RR by Anonymous Referee #1 (17 Sep 2026)
ED: Publish subject to minor revisions (review by editor) (21 Sep 2026) by Mario Hoppema
AR by Ivica Vilibić on behalf of the Authors (15 Oct 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (27 Oct 2026) by Mario Hoppema
AR by Ivica Vilibić on behalf of the Authors (05 Nov 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (06 Nov 2026) by Mario Hoppema
AR by Ivica Vilibić on behalf of the Authors (08 Nov 2026)
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Short summary
The Adriatic Sea has become warmer and saltier over the past two decades, and the change is fastest at depth: below 700 m it now warms about six times faster than the rest of the Mediterranean. Using 75 years of ship and float measurements, we show that salty layers at the sea surface became common after 2014 and that the salty intermediate water no longer sits at one depth. These changes may alter how oxygen and nutrients reach the deep sea.
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