Chapter
Dec 31, 2015
Wave Reflection from Undulating Seabed Topography
Publication: Coastal Engineering 1982
Abstract
The results of experiments are described which show that surface waves may experience a resonant interaction with undulations on the seabed. This interaction manifests itself in a strong reflection of incident wave energy when the wavelength of the bottom undulation is about half that of the surface wave. It is shown that such a mechanism might enable a region of undulating seabed topography (eg sand bars or sandwaves) to extend in an up-wave direction, into a region of otherwise plane bed.
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© 1982 American Society of Civil Engineers.
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Published online: Dec 31, 2015
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A D Heathershaw
Institute of Oceanographic Sciences, Crossway Taunton. TA1 2DW, UK.
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