2005
DOI: 10.2112/03-0048.1
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Sediment Transport in a Tidal Lagoon Subject to Varying Winds Evaluated with a Coupled Current-Wave Model

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Cited by 14 publications
(8 citation statements)
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“…Calibration parameters are fundamental together with boundary conditions and an appropriate combination of hydrodynamic forces [26,27]; usually a great effort is spent on researching a reliable reconstruction of the initial bed composition [8,28], but the same is not carried out for the variability of threshold bed shear stress for erosion, often assumed constant both in space and time [6,29], contrary to experimental evidence [30][31][32].…”
Section: Introductionmentioning
confidence: 99%
“…Calibration parameters are fundamental together with boundary conditions and an appropriate combination of hydrodynamic forces [26,27]; usually a great effort is spent on researching a reliable reconstruction of the initial bed composition [8,28], but the same is not carried out for the variability of threshold bed shear stress for erosion, often assumed constant both in space and time [6,29], contrary to experimental evidence [30][31][32].…”
Section: Introductionmentioning
confidence: 99%
“…Desde 1979, tras el trabajo pionero llevado a cabo por Grant y Madsen (1979), se han realizado distintos trabajos donde se estudia la interacción oleaje-marea, dentro de los que cabe destacar los siguientes: Davies y Lawrence (1995), Bender y Wong (1993), Kagan, et al (2003), Moon I.-J. (2005) y Bolaños- Sanchez, et al (2005) entre otros.…”
Section: Olabarrieta R Medina Y P Lomónacounclassified
“…1). The analysis of bedforms based on seismic profiles revealed that the area around Lister Deep is represented by a complex spatial pattern of the flood-and ebb-dominated subaqueous dunes (Boldreel et al, 2010).…”
Section: Introductionmentioning
confidence: 99%
“…The tidal residual circulation and asymmetric tidal cycles largely define the transport and accumulation of sediment and the distribution of bedforms in the bight (e.g. Boldreel et al, 2010;Burchard et al, 2008;Hayes, 1980;Nortier, 2004;Postma, 1967). Note that the tide entering the Wad-den Sea leaves ∼ 3.5 × 10 6 t yr −1 of suspended matter there according to Postma (1981).…”
Section: Introductionmentioning
confidence: 99%
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