Articles | Volume 8, issue 6
https://doi.org/10.5194/os-8-1085-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.Imbalance of energy and momentum source terms of the sea wave transfer equation for fully developed seas
Related subject area
Approach: Numerical Models | Depth range: Surface | Geographical range: All Geographic Regions | Phenomena: Surface Waves
Numerical modeling of surface wave development under the action of wind
Ocean Sci., 14, 453–470,
2018Cited articles
Alber, I. E.: The effect of randomness on the stability of two-dimensional surface wavetrains, P. Roy. Soc. Lond. Ser. A, 363, 525–546, 1978.
Ardhuin, F., Chapron, B., and Collard, F.: Observation of swell dissipation across oceans, Geophys. Res. Lett., 36, L06607, https://doi.org/10.1029/2008GL037030, 2009.
Ardhuin, F., Rogers, E., Babanin, A. V., Filipot, J. F., Magne, R., Roland, A., van der Westhuysen, A., Queffeulou, P., Lefevre, J. M., Aouf, L., and Collard, F.: Semi-empirical Dissipation Source Functions for Ocean Waves, Part I: Definition, Calibration, and Validation, J. Phys. Oceanogr., 40, 1917–1941, 2010.
Banner, M.: Equilibrium spectra of wind waves, J. Phys. Oceanogr., 20, 966–984, 1990.
Banner, M. L. and Morison, R. P.: Refined source terms in wind wave models with explicit wave breaking prediction, Part I: Model framework and validation against field data, Ocean Model., 33, 177–189, 2010.