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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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Cited articles  
Badulin, S., Babanin, A. V., Resio, D. T., and Zakharov, V.: Weakly turbulent laws of wind-wave growth, J. Fluid Mech., 591, 339–378, 2007.
Zakharov, V. E. and Badulin, S. I: The generalized Phillips' spectra and new dissipation function for wind-driven seas, arXiv:1212.0963v2 [physics.ao-ph], 1–16, https://arxiv.org/abs/1212.0963v2, 2015.
Badulin, S. I., Pushkarev, A. N., Resio, D., and Zakharov, V. E.: Self-similarity of wind-driven seas, Nonlin. Proc. Geoph., 12, 891–945, https://doi.org/10.5194/npg-12-891-2005, 2005.
Badulin, S. I., Pushkarev, A. N., Resio, D., and Zakharov, V. E.: Self-similarity of wind-driven sea, Nonlinear Proc. Geoph., 12, 891–945, 2005.
Balk, A. M.: On the Kolmogorov–Zakharov spectra of weak turbulence, Physica D, 139, 137–157, 2000.
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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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