Hostname: page-component-5c6d5d7d68-txr5j Total loading time: 0 Render date: 2024-08-08T01:18:06.238Z Has data issue: false hasContentIssue false

Resonant scattering of edge waves by longshore periodic topography: finite beach slope

Published online by Cambridge University Press:  25 May 1999

YONGZE CHEN
Affiliation:
Center for Coastal Studies, Scripps Institution of Oceanography, La Jolla, CA 92093, USA
R. T. GUZA
Affiliation:
Center for Coastal Studies, Scripps Institution of Oceanography, La Jolla, CA 92093, USA

Abstract

The resonant scattering of low-mode progressive edge waves by small-amplitude longshore periodic depth perturbations superposed on a plane beach has recently been investigated using the shallow water equations (Chen & Guza 1998). Coupled evolution equations describing the variations of edge wave amplitudes over a finite-size patch of undulating bathymetry were developed. Here similar evolution equations are derived using the full linear equations, removing the shallow water restriction of small (2N + 1)θ, where N is the maximum mode number considered and θ is the unperturbed planar beach slope angle. The present results confirm the shallow water solutions for vanishingly small (2N + 1)θ and allow simple corrections to the shallow water results for small but finite (2N + 1)θ. Additionally, multi-wave scattering cases occurring only when (2N + 1)θ = O(1) are identified, and detailed descriptions are given for the case involving modes 0, 1, and 2 that occurs only on a steep beach with θ = π/12.

Type
Research Article
Copyright
© 1999 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)