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Edge wave

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Surface gravity wave fixed by refraction against a rigid boundary, often a shoaling beach

Example of the surface elevation of a progressive edge wave

Influid dynamics, anedge wave is asurface gravity wave fixed byrefraction against a rigid boundary, often ashoaling beach. Progressive edge waves travel along this boundary, varyingsinusoidally along it and diminishingexponentially in the offshore direction.^[1]

References

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^Lamb, Horace (1932),Hydrodynamics, Cambridge:Cambridge University Press, p. 446,ISBN 0-521-45868-4{{citation}}:ISBN / Date incompatibility (help)

Ursell, F. (1952), "Edge waves on a sloping beach",Proceedings of the Royal Society of London. Series A, Mathematical and Physical Sciences,214 (1116):79–97,Bibcode:1952RSPSA.214...79U,doi:10.1098/rspa.1952.0152,S2CID 122032422
Miles, J.W. (1989), "Edge waves on a gently sloping beach",Journal of Fluid Mechanics,199:125–131,Bibcode:1989JFM...199..125M,doi:10.1017/S0022112089000315,S2CID 122744100
Chapman, C.J. (2001), "Energy paths in edge waves",Journal of Fluid Mechanics,426 (1):135–154,Bibcode:2001JFM...426..135C,doi:10.1017/S0022112000002184,S2CID 119424411

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