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Semi-empirical dissipation source functions for ocean waves: part I: definition, calibration and validation
List of Titles
Semi-empirical dissipation source functions for ocean waves: part I: definition, calibration and validation
Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.3/94456
- Title
- Semi-empirical dissipation source functions for ocean waves: part I: definition, calibration and validation
- Author(s)
- Ardhuin, Fabrice; Rogers, Erick; Babanin, Alexander V.; Filipot, Jean-Francois; Magne, Rudy; Roland, Aaron; van der Westhuysen, Andre; Queffeulou, Pierre; Lefevre, Jean-Michel; Aouf, Lofti; Collard, Fabrice
- Abstract
- New parameterizations for the spectral dissipation of wind-generated waves are proposed. The rates of dissipation have no predetermined spectral shapes and are functions of the wave spectrum and wind speed and direction, in a way consistent with observations of wave breaking and swell dissipation properties. Namely, the swell dissipation is nonlinear and proportional to the swell steepness, and dissipation due to wave breaking is nonzero only when a nondimensional spectrum exceeds the threshold at which waves are observed to start breaking. An additional source of short-wave dissipation is introduced to represent the dissipation of short waves due to longer breaking waves. A reduction of the wind-wave generation of short waves is meant to account for the momentum flux absorbed by longer waves. These parameterizations are combined and calibrated with the discrete interaction approximation for the nonlinear interactions. Parameters are adjusted to reproduce observed shapes of directional wave spectra, and the variability of spectral moments with wind speed and wave height. The wave energy balance is verified in a wide range of conditions and scales, from the global ocean to coastal settings. Wave height, peak and mean periods, and spectral data are validated using in situ and remote sensing data. Some systematic defects are still present, but, overall, the parameterizations probably yield the most accurate estimates of wave parameters to date. Perspectives for further improvement are also given.
- Publication type
- Journal article
- Research centre
- Swinburne University of Technology. Faculty of Engineering and Industrial Sciences
- Source
- Journal of Physical Oceanography, Vol. 40, no. 9 (Sep 2010), pp. 1917-1941
- Publication year
- 2010
- FOR Code(s)
- 0405 Oceanography
- Keyword(s)
- Oceanic waves; Parameterisation; Wind
- Publisher
- American Meteorological Society
- ISSN
- 0022-3670
- Publisher URL
- http://dx.doi.org/10.1175/2010JPO4324.1
- Copyright
- Copyright © 2010 American Meteorological Society. The published version of the paper is reproduced here in accordance with the copyright policy of the publisher.
- Full text

- Peer reviewed


