2008
DOI: 10.1016/j.geomorph.2007.10.013
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Relation between beachface morphology and wave climate at Trafalgar beach (Cádiz, Spain)

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Cited by 33 publications
(22 citation statements)
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“…Therefore, a broad number of coastal forms and nearshore processes can be monitored using remote techniques. For instance, researchers have used video images to extract beach and nearshore bathymetry (Stockdon and Holman, 2000;Aarninkhof et al, 2003), the nearshore hydrodynamics (Chickadel et al, 2003), as well as to unravel the formation and displacement of sand bars (Lippman and Holman, 1989;Ojeda, 2008;Ruessink et al, 2000) or the beachface morphodynamics (Almar et al, 2008;Ortega-Sánchez et al, 2007). The capabilities and functionality of video-based costal monitoring systems are evolving rapidly; more so with the CoastView project that highlighted and standardized the possibilities and future trends of these systems for coastal zone or navigational channels management Turner and Anderson, 2007;Koningsveld et al, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, a broad number of coastal forms and nearshore processes can be monitored using remote techniques. For instance, researchers have used video images to extract beach and nearshore bathymetry (Stockdon and Holman, 2000;Aarninkhof et al, 2003), the nearshore hydrodynamics (Chickadel et al, 2003), as well as to unravel the formation and displacement of sand bars (Lippman and Holman, 1989;Ojeda, 2008;Ruessink et al, 2000) or the beachface morphodynamics (Almar et al, 2008;Ortega-Sánchez et al, 2007). The capabilities and functionality of video-based costal monitoring systems are evolving rapidly; more so with the CoastView project that highlighted and standardized the possibilities and future trends of these systems for coastal zone or navigational channels management Turner and Anderson, 2007;Koningsveld et al, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…Recently, many studies have been published on this method which has enabled significant progress in the knowledge of both intertidal and subtidal bar systems Ruessink, 2003a, 2003b;Ranasinghe et al, 2004;Quartel et al, 2007Quartel et al, , 2008. In particular, the role of morphologic feedback (Wright et al, 1985;Ruessink and Terwindt, 2000;Plant et al, 2001;Quartel et al, 2008;Ortega-Sanchez et al, 2008) and possible coupling between the systems have been investigated, as well as the influence of tide on the type, intensity and duration of the wave processes operating on the cross-shore profile (Masselink and Turner, 1999;Masselink et al, 2006;Reichmüth and Anthony, 2007;Price and Ruessink, 2008). Nevertheless, most of these studies concern micro-and meso-tidal environments and there are still knowledge gaps concerning meso-, macro-, and mega-tidal environments.…”
Section: Introductionmentioning
confidence: 99%
“…The southwestern area of the Gulf of Cádiz is one of the few locations along the southern coast of Spain where it is feasible to install a WEC array 55 due to its wide continental shelf (30 km), relatively low depths and mild slopes (Ortega-Sánchez et al, 2008), with the shelf-break at approximately 120 m water depth (Fig. 1a-b).…”
Section: Study Sitementioning
confidence: 99%
“…The astronomical tide is semi-diurnal with tidal ranges between 1.2 m and 3.8 m (Ortega-Sánchez et al, 2008). Wave data from SIMAR point 5034009…”
Section: Study Sitementioning
confidence: 99%