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dc.contributor.authorVan den Berg, Niels
dc.contributor.authorFalqués Serra, Albert
dc.contributor.authorRibas Prats, Francesca
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament de Física Aplicada
dc.date.accessioned2011-04-08T07:19:44Z
dc.date.available2011-04-08T07:19:44Z
dc.date.created2010
dc.date.issued2010
dc.identifier.citationVan den Berg, N.; Falqués, A.; Ribas, F. Shoreline sand waves and beach nourishments. A: International Conference on Coastal Engineering. "32nd International Conference on Coastal Engineering". Coastal Engineering Research Council, 2010, p. 1-10.
dc.identifier.urihttp://hdl.handle.net/2117/12312
dc.description.abstractThe effects of the feedback between the changing coastal morphology and the wavefield on the generation and propagation of large scale (O(1-10 km)) shoreline sand waves is examined with a quasi-2D morphodynamic model. Traditional shoreline change models do not include this feedback and are only able to describe diffusion of shoreline sand waves and furthermore they are unable to describe migration. It is found with the present model that if there is a dominant littoral drift, the feedback causes downdrift migration of coastline features no matter if they grow or decay. Consistently with previous studies, simulations show that a rectilinear coastline becomes unstable and sand waves tend to grow spontaneously from random perturbations, if the wave incidence angle is larger then about 42º (θc) at the depth of closure (high angle wave instability). The initial wavelengths at which the sand waves develop are 2-3 km and this is similar to previous linear stability analysis. The implications of high angle wave instability for beach nourishments are investigated. The nourished shoreline retreats initially due to cross-shore transport because the nourished profile is steeper than the equilibrium profile. When a dominant littoral drift is present, the nourishment also migrates downdrift. If the wave angle at the depth of closure is below θc the alongshore transport contributes to the diffusion of the nourishment. However, if the angle is above θc (constant high angle wave conditions) the diffusion is reversed and the nourishment can trigger the formation of a shoreline sand wave train. Numerical experiments changing the proportion of "high angle waves" and "low angle waves" in the wave climate show that relatively small proportions of low angle waves slow down the growth of sand waves. These simulations with more realistic wave climates show shoreline sand waves that migrate downdrift maintaining more or less the same amplitude for years.
dc.format.extent10 p.
dc.language.isoeng
dc.publisherCoastal Engineering Research Council
dc.rightsAttribution 3.0 Spain
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/es/
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Geologia::Oceanografia
dc.subject.lcshShorelines -- Research
dc.subject.lcshSand waves -- Mathematical models
dc.titleShoreline sand waves and beach nourishments
dc.typeConference report
dc.contributor.groupUniversitat Politècnica de Catalunya. DF - Dinàmica No Lineal de Fluids
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttps://journals.tdl.org/ICCE/article/view/1310/pdf_316
dc.rights.accessOpen Access
local.identifier.drac5272624
dc.description.versionPostprint (published version)
local.citation.authorVan den Berg, N.; Falqués, A.; Ribas, F.
local.citation.contributorInternational Conference on Coastal Engineering
local.citation.publicationName32nd International Conference on Coastal Engineering
local.citation.startingPage1
local.citation.endingPage10


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Attribution 3.0 Spain
Except where otherwise noted, content on this work is licensed under a Creative Commons license : Attribution 3.0 Spain