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Forcing a three-dimensional, hydrostatic, primitive-equation model for application in the surf zone : 2. application to DUCK94

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Field Value
Title Forcing a three-dimensional, hydrostatic, primitive-equation model for application in the surf zone : 2. application to DUCK94
Names Newberger, P. A. (creator)
Allen, John S. (creator)
Date Issued 2007-08-31 (iso8601)
Note copyrighted by American Geophysical Union
Abstract A three-dimensional primitive-equation model for application to the nearshore surf
zone has been developed. This model, an extension of the Princeton Ocean Model (POM),
predicts the wave-averaged circulation forced by breaking waves. All of the features of the
original POM are retained in the extended model so that applications can be made to
regions where breaking waves, stratification, rotation, and wind stress make significant
contributions to the flow behavior. In this study we examine the effects of breaking waves
and wind stress. The nearshore POM circulation model is embedded within the NearCom
community model and is coupled with a wave model. This combined modeling system is
applied to the nearshore surf zone off Duck, North Carolina, during the DUCK94 field
experiment of October 1994. Model results are compared to observations from this
experiment, and the effects of parameter choices are examined. A process study examining
the effects of tidal depth variation on depth-dependent wave-averaged currents is carried
out. With identical offshore wave conditions and model parameters, the strength and
spatial structure of the undertow and of the alongshore current vary systematically with
water depth. Some three-dimensional solutions show the development of shear instabilities
of the alongshore current. Inclusion of wave-current interactions makes an appreciable
difference in the characteristics of the instability.
Genre Article
Identifier Allen, J. S., and Newberger, P. A. (2007), Forcing a three-dimensional, hydrostatic, primitive-equation model for application in the surf zone: 2. application to DUCK94, J. Geophys. Res., 112, C08019.

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