2018
DOI: 10.3390/w10101348
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On the Wave Bottom Shear Stress in Shallow Depths: The Role of Wave Period and Bed Roughness

Abstract: Lagoons and coastal semi-enclosed basins morphologically evolve depending on local waves, currents, and tidal conditions. In very shallow water depths, typical of tidal flats and mudflats, the bed shear stress due to the wind waves is a key factor governing sediment resuspension. A current line of research focuses on the distribution of wave shear stress with depth, this being a very important aspect related to the dynamic equilibrium of transitional areas. In this work a relevant contribution to this study is… Show more

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Cited by 21 publications
(27 citation statements)
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“…The hydrodynamic model is based on classical 2DH shallow water equations, which include: turbulent fluxes treated according to the Smagorinsky approach as in the study of Pascolo et al [38], the forcings due to wind shear stress and radiation stress, and the mean bottom shear stress, which is influenced by both current and wave motion as pointed out by Soulsby [39,40]. The resulting differential equation system is integrated with a finite volume method which is able to represent phenomena such as the propagation of water front over a dry bed, which regularly occurs in lagoons and coastal environments at each tidal cycle, with the submergence and emergence of saltmarshes and beaches.…”
Section: Numerical Model and Computational Domainsmentioning
confidence: 99%
“…The hydrodynamic model is based on classical 2DH shallow water equations, which include: turbulent fluxes treated according to the Smagorinsky approach as in the study of Pascolo et al [38], the forcings due to wind shear stress and radiation stress, and the mean bottom shear stress, which is influenced by both current and wave motion as pointed out by Soulsby [39,40]. The resulting differential equation system is integrated with a finite volume method which is able to represent phenomena such as the propagation of water front over a dry bed, which regularly occurs in lagoons and coastal environments at each tidal cycle, with the submergence and emergence of saltmarshes and beaches.…”
Section: Numerical Model and Computational Domainsmentioning
confidence: 99%
“…In the presence of a more irregular bottom, characterized by bedforms (uneven granulometry with coexistence of sand and mud, and vegetation), the wave friction factor can considerably increase. This result was achieved by the authors in a previous study [45], performing a numerical generation process by means of the third generation spectral model SWAN [61], based on the complete wave action balance equation.…”
Section: Tidal Flat Morphodynamics: Some Preliminary Considerationsmentioning
confidence: 93%
“…The generation process of wind waves on shallow depths leads to quite different characteristics from offshore waves developed on deep waters, as the friction dissipation severely restricts the maximum value that wave heights and periods can reach [3,45]. This particular aspect has been verified both experimentally and numerically and it has led to a set of equations formulated for wave forecasting in shallow water [43,59].…”
Section: Tidal Flat Morphodynamics: Some Preliminary Considerationsmentioning
confidence: 99%
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“…Models enable complex underlying processes to be captured, and facilitate the analysis of interrelationships between variables in cases with limited data [2]. Modeling has major applications in fields such as hydrology, maritime and coastal studies [3,4], river hydraulics [5] and water quality [6].…”
Section: Introductionmentioning
confidence: 99%