Refraction of surface gravity waves by shear waves
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Authors
Henderson, Stephen M.
Guza, R. T.
Elgar, Steve
Herbers, T.H.C.
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Date of Issue
2006-04
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American Meteorological Society
Language
en_US
Abstract
Previous field observations indicate that the directional spread of swell-frequency (nominally 0.1 Hz) surface gravity waves increases during shoreward propagation across the surf zone. This directional broadening contrasts with the narrowing observed seaward of the surf zone and predicted by Snell’s law for bathymetric refraction. Field-observed broadening was predicted by a new model for refraction of swell by lower-frequency (nominally 0.01 Hz) current and elevation fluctuations. The observations and the model suggest that refraction by the cross-shore currents of energetic shear waves contributed substantially to the observed broadening.
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Article
Description
The article of record as published may be found at https://doi.org/10.1175/JPO2890.1
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Funding was provided by the Office
of Naval Research, the National Science Foundation,
and the National Ocean Partnership Program.
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Citation
Journal of Physical Oceanography 36 (2006): 629-635, doi:10.1175/JPO2890.1.
Journal of Physical Oceanography 36 (2006): 629-635
Journal of Physical Oceanography 36 (2006): 629-635