Changes in extreme regional sea level under global warming

Brunnabend, S.-E.; Dijkstra, H. A.; Kliphuis, M. A.; Bal, H. E.; Seinstra, F.; van Werkhoven, B.; Maassen, J.; van Meersbergen, M.

doi:https://doi.org/10.5194/os-13-47-2017

Articles | Volume 13, issue 1

https://doi.org/10.5194/os-13-47-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/os-13-47-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 13, issue 1

Research article

|

20 Jan 2017

Research article |

| 20 Jan 2017

Changes in extreme regional sea level under global warming

S.-E. Brunnabend, H. A. Dijkstra, M. A. Kliphuis, H. E. Bal, F. Seinstra, B. van Werkhoven, J. Maassen, and M. van Meersbergen

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Final revised paper (published on 20 Jan 2017)
Preprint (discussion started on 02 Aug 2016)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'Review of the manuscript by Brunnabend et al.', Anonymous Referee #1, 02 Sep 2016
- AC1: 'Response to comments by referee 1', Sandra-Esther Brunnabend, 10 Nov 2016
RC2: 'Review coments', Anonymous Referee #2, 11 Oct 2016
- AC2: 'Response to comment by Referee 2', Sandra-Esther Brunnabend, 10 Nov 2016

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Sandra-Esther Brunnabend on behalf of the Authors (07 Dec 2016) Author's response Manuscript

ED: Publish subject to technical corrections (17 Dec 2016) by Matthew Hecht

AR by Sandra-Esther Brunnabend on behalf of the Authors (20 Dec 2016) Author's response Manuscript

Short summary

An important contribution to future changes in regional sea level extremes is due to the changes in intrinsic ocean variability, in particular ocean eddies. Here, we study a scenario of future dynamic sea level (DSL) extremes using a strongly eddying version of the Parallel Ocean Program. Changes in 10-year return time DSL extremes are very inhomogeneous over the globe and are related to changes in ocean currents and corresponding regional shifts in ocean eddy pathways.