An explicit method for the nonlinear int
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Dorian Fructus; John Grue
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Article
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2007
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Elsevier Science
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English
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A fully nonlinear and fully dispersive method for the interaction between free surface waves and a variable bottom topography in space and time in three dimensions is derived. A Green function potential formulation expresses the normal velocity of the free surface in terms of the bathymetry and its