1998
DOI: 10.1016/s0378-3839(98)00028-3
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Hyperbolic mild-slope equations extended to account for rapidly varying topography

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Cited by 49 publications
(30 citation statements)
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“…These errors in the MSE solution are primarily due to the bottom curvature induced by the slope discontinuity at both ends of the transitional slope. Lee et al (1998) found the mild-slope approximation to be even more limiting when waves of a range of relative water depths kh were considered. Finally, Kirby and Misra (unpublished manuscript) argued that the MSE is not the correct leading-order approximation even for a slowly varying sea bed.…”
Section:   Kh Hmentioning
confidence: 99%
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“…These errors in the MSE solution are primarily due to the bottom curvature induced by the slope discontinuity at both ends of the transitional slope. Lee et al (1998) found the mild-slope approximation to be even more limiting when waves of a range of relative water depths kh were considered. Finally, Kirby and Misra (unpublished manuscript) argued that the MSE is not the correct leading-order approximation even for a slowly varying sea bed.…”
Section:   Kh Hmentioning
confidence: 99%
“…For practical applications, where our interest is ultimately in the shoreline response to the presence of localized bottom features, it is also necessary to choose a model that can handle non-idealized bathymetries. For these reasons, we have chosen the finite difference formulation of the MMSE as given by Lee et al (1998). Since this model solves the equations in hyperbolic form, it also has the advantage of requiring shorter computational times as compared to models using the elliptical form.…”
Section:   Kh Hmentioning
confidence: 99%
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