DOI: 10.3990/1.9789036542456
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Sand transport processes in the surf and swash zones

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Cited by 7 publications
(5 citation statements)
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References 182 publications
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“…The mean rotation angle for each run was found to match closely the local bed slope obtained from the bed profile measurements, which supports the validity of the transformation procedure. The velocity measurements were de-noised and decomposed into time-averaged (u ̅, w ̅), periodic (ũ, w) and turbulent (u', w') components; the latter component was used to quantify the turbulent kinetic energy k (van der Zanden et al, 2016).…”
Section: Data Treatmentmentioning
confidence: 99%
“…The mean rotation angle for each run was found to match closely the local bed slope obtained from the bed profile measurements, which supports the validity of the transformation procedure. The velocity measurements were de-noised and decomposed into time-averaged (u ̅, w ̅), periodic (ũ, w) and turbulent (u', w') components; the latter component was used to quantify the turbulent kinetic energy k (van der Zanden et al, 2016).…”
Section: Data Treatmentmentioning
confidence: 99%
“…Interacting factors such as bathymetry, coastline typology, presence or absence of sea and land breezes, waves, etc., concur in making the stranding processes complex. The dominant hydrodynamics in coastal waters controlling the transport of plastic objects in swash and surf zones differ significantly from the hydrodynamics occurring in the open ocean [ 40 , 41 ]. The restraining effect of a near-coastal boundary or shallow bottom topography may affect the drift response to local wind forcing [ 42 ].…”
Section: Introductionmentioning
confidence: 99%
“…Figure 9. Conceptual drawing of the cross-shore wave related processes (adapted from van der Zanden (2016) [27]), environmental parameters measured and the macrobenthic species identified as indicator species for the morphological features.…”
Section: Discussionmentioning
confidence: 99%
“…Eventually, the wave breaks at the seaward slope or crest of the bar, leading to a reduction in wave energy and wave height [26]. The turbulence induced by the breaking waves increases the amount of sediment in suspension [27]. After the wave is broken the wave continues as a surface roller in shoreward direction.…”
Section: Introductionmentioning
confidence: 99%