Articles | Volume 13, issue 3
https://doi.org/10.5194/os-13-443-2017
https://doi.org/10.5194/os-13-443-2017
Research article
 | 
12 Jun 2017
Research article |  | 12 Jun 2017

Quantifying the impact of basin dynamics on the regional sea level rise in the Black Sea

Arseny A. Kubryakov, Sergey V. Stanichny, and Denis L. Volkov

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Kubryakov Arseny on behalf of the Authors (20 Dec 2016)  Author's response
ED: Referee Nomination & Report Request started (03 Jan 2017) by John M. Huthnance
RR by Anonymous Referee #1 (17 Jan 2017)
ED: Reconsider after major revisions (24 Jan 2017) by John M. Huthnance
AR by Kubryakov Arseny on behalf of the Authors (03 Mar 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (17 Mar 2017) by John M. Huthnance
ED: Publish subject to minor revisions (Editor review) (07 Apr 2017) by John M. Huthnance
AR by Anna Wenzel on behalf of the Authors (18 Apr 2017)  Author's response    Manuscript
ED: Publish subject to technical corrections (21 Apr 2017) by John M. Huthnance
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Short summary
The Black Sea dynamics impact on the local sea level rise. In recent decades, the increase of the wind curl induced the intensification of the cyclonic circulation and divergence in the basin center. As a result, the sea level rise in the coastal areas is 1.5–2 times higher than in the basin center. Additional heterogeneity of sea level trends is related to the changes of the mesoscale dynamics. The large-scale dynamic sea level and its rise can be estimated using atmospheric reanalysis data.