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Authordc.contributor.authorLe Roux, Jacobus 
Admission datedc.date.accessioned2010-01-27T20:31:59Z
Available datedc.date.available2010-01-27T20:31:59Z
Publication datedc.date.issued2008-08
Cita de ítemdc.identifier.citationCOASTAL ENGINEERING Volume: 55 Issue: 9 Pages: 701-703 Published: AUG 2008en_US
Identifierdc.identifier.issn0378-3839
Identifierdc.identifier.other10.1016/j.coastaleng.2008.02.003
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/125262
Abstractdc.description.abstractAiry waves have a sinusoidal profile in deep water that can be modeled by a time series at any point x and time t, given by eta(x,t)=(H-o/2) cos[2 pi x/L-o-2 pi t/T-w], where H-o is the deepwater height, L-o is the deepwater wavelength, and T-w is the wave period. However, as these waves approach the shore they change in form and dimension so that this equation becomes invalid. A method is presented to reconstruct the wave profile showing the correct wavelength, wave height, wave shape, and displacement of the water surface with respect to the still water level for any water depth.en_US
Lenguagedc.language.isoenen_US
Publisherdc.publisherELSEVIERen_US
Keywordsdc.subjectSHALLOW-WATERen_US
Títulodc.titleProfiles of fully developed (Airy) waves in different water depthsen_US
Document typedc.typeArtículo de revista


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