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contributor authorAlves, Jose Henrique G. M.
contributor authorBanner, Michael L.
date accessioned2017-06-09T14:55:45Z
date available2017-06-09T14:55:45Z
date copyright2003/06/01
date issued2003
identifier issn0022-3670
identifier otherams-29878.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4167153
description abstractA new formulation of the spectral dissipation source term Sds for wind-wave modeling applications is investigated. This new form of Sds is based on a threshold behavior of deep-water wave-breaking onset associated with nonlinear wave-group modulation. It is expressed in terms of the azimuth-integrated spectral saturation, resulting in a nonlinear dependence of dissipation rates on the local wave spectrum. Validation of the saturation-based Sds is made against wave field parameters derived from observations of fetch-limited wind-wave evolution. Simulations of fetch-limited growth are made with a numerical model featuring an exact nonlinear form of the wave?wave-interactions source term Snl. For reference, the performance of this saturation-based Sds is compared with the performance of the wave-dissipation source-term parameterization prescribed for the Wave Modeling Project (WAM) wind-wave model. Calculations of integral spectral parameters using the saturation-based model for Sds agree closely with fetch-limited observations. It is also shown that the saturation-based Sds can be readily adjusted to accommodate several commonly used parameterizations of the wind input source term Sin. Also, this new form of Sds provides greater flexibility in controlling the shape of the wave spectrum in the short gravity-wave region.
publisherAmerican Meteorological Society
titlePerformance of a Saturation-Based Dissipation-Rate Source Term in Modeling the Fetch-Limited Evolution of Wind Waves
typeJournal Paper
journal volume33
journal issue6
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(2003)033<1274:POASDS>2.0.CO;2
journal fristpage1274
journal lastpage1298
treeJournal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 006
contenttypeFulltext


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