Three-dimensional Green's function for harmonic water waves over a bottom topography with different depths at infinity

Belibassakis, KA; Athanassoulis, GA

dc.contributor.author	Belibassakis, KA	en
dc.contributor.author	Athanassoulis, GA	en
dc.date.accessioned	2014-03-01T01:21:39Z
dc.date.available	2014-03-01T01:21:39Z
dc.date.issued	2004	en
dc.identifier.issn	0022-1120	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/16291
dc.subject	Green Function	en
dc.subject	Three Dimensional	en
dc.subject	Water Waves	en
dc.subject.classification	Mechanics	en
dc.subject.classification	Physics, Fluids & Plasmas	en
dc.subject.other	Fourier transforms	en
dc.subject.other	Green's function	en
dc.subject.other	Harmonic analysis	en
dc.subject.other	Water waves	en
dc.subject.other	Monochromatic point source	en
dc.subject.other	Variable-bathymetry regions	en
dc.subject.other	Fluid mechanics	en
dc.subject.other	fluid mechanics	en
dc.subject.other	Green function	en
dc.subject.other	seafloor roughness	en
dc.subject.other	water wave	en
dc.subject.other	wave propagation	en
dc.subject.other	fluid mechanics	en
dc.subject.other	Green function	en
dc.subject.other	seafloor	en
dc.subject.other	water wave	en
dc.subject.other	wave propagation	en
dc.title	Three-dimensional Green's function for harmonic water waves over a bottom topography with different depths at infinity	en
heal.type	journalArticle	en
heal.identifier.primary	10.1017/S0022112004009516	en
heal.identifier.secondary	http://dx.doi.org/10.1017/S0022112004009516	en
heal.language	English	en
heal.publicationDate	2004	en
heal.abstract	The three-dimensional Green's function of water waves in variable-bathymetry regions, associated with the problem of propagation of water waves emitted from a monochromatic point source, is derived and studied. The solution is of interest in its own right but also provides useful information for the formulation and treatment of complex wave-body-seabed interaction problems in variable-bathymetry regions, especially as regards the hydrodynamic characteristics of large structures installed in the nearshore and coastal environment. Assuming a parallel-contour bathymetry, with a continuous depth function of the form h(x, y) = h(x), attaining constant, but possibly different, values at the semi-infinite regions x < a and x > b, the problem is reduced to a two-dimensional one, by using Fourier transform. The transformed problem is treated by applying domain decomposition and reformulating it as a transmission problem in the finite domain containing the bottom irregularity. An appropriate decomposition of the wave potential is introduced, permitting the singular part to be solved analytically, and the problem for the regular part to be reformulated as a variational problem. An enhanced local-mode series representation is used for the regular wave potential in the variable-bathymetry region, including the propagating mode, the sloping-bottom mode (see Athanassoulis & Belibassakis 1999), and a number of evanescent modes. Using this representation, in conjunction with the variational principle, a forced system of horizontal coupled-mode equations is derived for the determination of the complex modal-amplitude functions of the regular wave potential. This system is numerically solved by using a second-order central finite-difference scheme. The source-generated water-wave potential is, finally, obtained by an efficient numerical Fourier inversion based on FFT. Numerical results tire presented and discussed for various bottom topographies, including smooth but steep underwater trenches and ridges, putting emphasis on the identification of the important features of the near- and far-field patterns on the horizontal plane and on the vertical plane containing the point source. Characteristic patterns of trapped (well-localized) wave propagation over ridges are predicted and discussed. © 2004 Cambridge University Press.	en
heal.publisher	CAMBRIDGE UNIV PRESS	en
heal.journalName	Journal of Fluid Mechanics	en
dc.identifier.doi	10.1017/S0022112004009516	en
dc.identifier.isi	ISI:000222871100013	en
dc.identifier.volume	510	en
dc.identifier.issue	510	en
dc.identifier.spage	267	en
dc.identifier.epage	302	en