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Nonlinear Processes in Geophysics An interactive open-access journal of the European Geosciences Union
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Volume 24, issue 4
Nonlin. Processes Geophys., 24, 581–597, 2017
https://doi.org/10.5194/npg-24-581-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Nonlin. Processes Geophys., 24, 581–597, 2017
https://doi.org/10.5194/npg-24-581-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 09 Oct 2017

Research article | 09 Oct 2017

Balanced source terms for wave generation within the Hasselmann equation

Vladimir Zakharov et al.
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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 Anna Wenzel on behalf of the Authors (16 Mar 2017)  Author's response    Manuscript
ED: Reconsider after major revisions (further review by Editor and Referees) (18 Mar 2017) by Victor Shrira
ED: Referee Nomination & Report Request started (21 Mar 2017) by Victor Shrira
RR by Anonymous Referee #2 (29 Mar 2017)
ED: Reconsider after major revisions (further review by Editor and Referees) (30 Mar 2017) by Victor Shrira
AR by Andrei Pushkarev on behalf of the Authors (11 Jun 2017)  Author's response    Manuscript
ED: Reconsider after major revisions (further review by Editor and Referees) (13 Jun 2017) by Victor Shrira
ED: Referee Nomination & Report Request started (19 Jun 2017) by Victor Shrira
RR by Anonymous Referee #2 (01 Jul 2017)
ED: Publish subject to minor revisions (further review by Editor) (02 Jul 2017) by Victor Shrira
AR by Andrei Pushkarev on behalf of the Authors (07 Aug 2017)  Author's response    Manuscript
ED: Publish subject to technical corrections (16 Aug 2017) by Victor Shrira
Publications Copernicus
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Short summary
The Hasselmann equation (HE) is the basis of modern surface ocean wave prediction models. Currently, they operate in the black box with the tuning knobs modes, since there is no consensus on universal wind input and wave-breaking dissipation source terms, and require re-tuning for different boundary and external conditions. We offer a physically justified framework able to reproduce theoretical properties of the HE and experimental field data without re-tuning of the model.
The Hasselmann equation (HE) is the basis of modern surface ocean wave prediction models....
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