A model of Black Sea circulation with strait exchange (2008–2018)

Gunduz, Murat; Özsoy, Emin; Hordoir, Robinson

doi:https://doi.org/10.5194/gmd-13-121-2020

Articles | Volume 13, issue 1

https://doi.org/10.5194/gmd-13-121-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/gmd-13-121-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 13, issue 1

Model description paper

|

16 Jan 2020

Model description paper |

| 16 Jan 2020

A model of Black Sea circulation with strait exchange (2008–2018)

Murat Gunduz, Emin Özsoy, and Robinson Hordoir

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Final revised paper (published on 16 Jan 2020)
Preprint (discussion started on 30 Aug 2019)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review of manuscript entitled "A Model of Black Sea Circulation with Strait Exchange (2008–2018)"', Anonymous Referee #1, 23 Sep 2019
- AC1: 'Response to Referee 1', Murat Gunduz, 22 Nov 2019
RC2: 'Referee Comment on model description paper', Anonymous Referee #2, 08 Oct 2019
- AC2: 'Response to Referee 2', Murat Gunduz, 22 Nov 2019
RC3: 'Review of manuscript entitled “A Model of Black Sea Circulation with Strait Exchange (2008-2018)” by Murat Gunduz, Emin Özsoy and Robinson Hordoir', Anonymous Referee #3, 08 Oct 2019
- AC3: 'Response to Referee 3', Murat Gunduz, 22 Nov 2019

Peer-review completion

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

AR by Murat Gunduz on behalf of the Authors (22 Nov 2019)

ED: Publish as is (01 Dec 2019) by R. Marsh

AR by Murat Gunduz on behalf of the Authors (09 Dec 2019)

Short summary

The Bosphorus exchange is of critical importance for hydrodynamics and hydroclimatology of the Black Sea. In this study, we report on the development of a medium-resolution circulation model of the Black Sea, making use of surface atmospheric forcing with high space and time resolution, climatic river fluxes and strait exchange, enabled by adding elementary details of strait and coastal topography and seasonal hydrology specified in an artificial box on the Marmara Sea side.