Please use this identifier to cite or link to this item: http://repository.umac.mo/handle/10692/916
Title: On mass transport of progressive edge waves
Authors: Mok, Kai Meng (莫啟明)
Yeh, Harry
Issue Date: Oct-1999
Publisher: American Institute of Physics
Citation: Physics of fluids, Oct. 1999, v. 11, no. 10, p. 2906-2924
Abstract: The boundary-layer solutions for progressive edge waves on a uniformly sloping beach are derived. The Larangian mass transport in the cross-shore direction is found to be caused by the viscous effect and it changes direction within the boundary layer. For validation of the theoretical model, laboratory experiments are performed. The measured mass transports of mode 0 and 1 edge waves are in good agreement with the theory qualitatively but not quantitatively. The discrepancies appear to be caused by the failure of the theory near the shoreline, where the boundary layer is no longer thin. The inviscid Stokes drift caused by the nonlinear interactions of different edge-wave modes within the potential flow field is also investigated theoretically and verified by experiments. It is found that near-shore circulation cells can be formed by the nonlinear interactions between differentprogressive edge-wave modes.
URI: http://hdl.handle.net/10692/916
ISSN: 1070-6631
Keywords: Boundary layer
Edge waves
Mass transport
Near-shore circulation
Nonlinear interactions
Stokes drift
Access: http://pof.aip.org/resource/1/phfle6/v11/i10/p2906_s1
Appears in Collections:OTHERS Journal Articles

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