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Due to the ongoing rise in sea level and increases in extreme wave climates, which consequently change the wave climate, coastal structures such as sea dikes and seawalls are exposed to severe and frequent sea storms. Even though much research related to wave–structure interactions has been carried out, it remains one of the most important and challenging topics in the field of coastal engineering. The recent publications in the Special Issue “Wave Interactions with Coastal Structures” in the Journal of Marine Science and Engineering include a wide range of research, including theoretical/mathematical, experimental, and numerical work related to the interaction between sea waves and coastal structures. These publications address conventional coastal hard structures in deep water zones as well as those located in shallow water zones, such as wave overtopping over shallow foreshores with apartment buildings on dikes. The research findings presented help to improve our knowledge of hydrodynamic processes, and the new approaches and developments presented here will be good benchmarks for future work.
Technology: general issues --- History of engineering & technology --- shallow waters --- wave energy --- coastal erosion --- beach restoration --- submerged breakwaters --- protected nourishments --- wave overtopping --- coastal safety --- flow velocity --- flow depth --- sea dikes --- overtopping reduction --- force reduction --- oblique waves --- storm return wall --- EurOtop manual --- validation --- wave modelling --- shallow foreshore --- dike-mounted vertical wall --- wave impact loads --- OpenFOAM --- average overtopping discharge --- individual volume --- overtopping flow depth --- overtopping flow velocity --- promenade --- vertical wall --- SWASH --- fluid–structure interaction --- waves --- smoothed particle hydrodynamics --- SPH --- Pont del Petroli --- storm Gloria --- inter-model comparison --- DualSPHysics --- wave pressure --- caisson breakwater --- stability --- RANS model --- solitary wave --- fully nonlinear wave --- three-dimensional wave --- partially submerged cylinder --- hollow circular cylinder --- tsunami --- wave --- bore --- flooding --- debris --- numerical modeling --- SPH–FEM coupling --- coastal structures --- n/a --- fluid-structure interaction --- SPH-FEM coupling
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Due to the ongoing rise in sea level and increases in extreme wave climates, which consequently change the wave climate, coastal structures such as sea dikes and seawalls are exposed to severe and frequent sea storms. Even though much research related to wave–structure interactions has been carried out, it remains one of the most important and challenging topics in the field of coastal engineering. The recent publications in the Special Issue “Wave Interactions with Coastal Structures” in the Journal of Marine Science and Engineering include a wide range of research, including theoretical/mathematical, experimental, and numerical work related to the interaction between sea waves and coastal structures. These publications address conventional coastal hard structures in deep water zones as well as those located in shallow water zones, such as wave overtopping over shallow foreshores with apartment buildings on dikes. The research findings presented help to improve our knowledge of hydrodynamic processes, and the new approaches and developments presented here will be good benchmarks for future work.
shallow waters --- wave energy --- coastal erosion --- beach restoration --- submerged breakwaters --- protected nourishments --- wave overtopping --- coastal safety --- flow velocity --- flow depth --- sea dikes --- overtopping reduction --- force reduction --- oblique waves --- storm return wall --- EurOtop manual --- validation --- wave modelling --- shallow foreshore --- dike-mounted vertical wall --- wave impact loads --- OpenFOAM --- average overtopping discharge --- individual volume --- overtopping flow depth --- overtopping flow velocity --- promenade --- vertical wall --- SWASH --- fluid–structure interaction --- waves --- smoothed particle hydrodynamics --- SPH --- Pont del Petroli --- storm Gloria --- inter-model comparison --- DualSPHysics --- wave pressure --- caisson breakwater --- stability --- RANS model --- solitary wave --- fully nonlinear wave --- three-dimensional wave --- partially submerged cylinder --- hollow circular cylinder --- tsunami --- wave --- bore --- flooding --- debris --- numerical modeling --- SPH–FEM coupling --- coastal structures --- n/a --- fluid-structure interaction --- SPH-FEM coupling
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Due to the ongoing rise in sea level and increases in extreme wave climates, which consequently change the wave climate, coastal structures such as sea dikes and seawalls are exposed to severe and frequent sea storms. Even though much research related to wave–structure interactions has been carried out, it remains one of the most important and challenging topics in the field of coastal engineering. The recent publications in the Special Issue “Wave Interactions with Coastal Structures” in the Journal of Marine Science and Engineering include a wide range of research, including theoretical/mathematical, experimental, and numerical work related to the interaction between sea waves and coastal structures. These publications address conventional coastal hard structures in deep water zones as well as those located in shallow water zones, such as wave overtopping over shallow foreshores with apartment buildings on dikes. The research findings presented help to improve our knowledge of hydrodynamic processes, and the new approaches and developments presented here will be good benchmarks for future work.
Technology: general issues --- History of engineering & technology --- shallow waters --- wave energy --- coastal erosion --- beach restoration --- submerged breakwaters --- protected nourishments --- wave overtopping --- coastal safety --- flow velocity --- flow depth --- sea dikes --- overtopping reduction --- force reduction --- oblique waves --- storm return wall --- EurOtop manual --- validation --- wave modelling --- shallow foreshore --- dike-mounted vertical wall --- wave impact loads --- OpenFOAM --- average overtopping discharge --- individual volume --- overtopping flow depth --- overtopping flow velocity --- promenade --- vertical wall --- SWASH --- fluid-structure interaction --- waves --- smoothed particle hydrodynamics --- SPH --- Pont del Petroli --- storm Gloria --- inter-model comparison --- DualSPHysics --- wave pressure --- caisson breakwater --- stability --- RANS model --- solitary wave --- fully nonlinear wave --- three-dimensional wave --- partially submerged cylinder --- hollow circular cylinder --- tsunami --- wave --- bore --- flooding --- debris --- numerical modeling --- SPH-FEM coupling --- coastal structures
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This document reports a following up of the EU-funded research project DURCWAVE (amending the Design criteria of URban defences in LECZs through Composite-modelling of WAVE overtopping under climate change scenarios). The role of FHR was an external advisor for the project. FHR exchanged the knowledge on overtopping design criteria and coastal management policy with Dr. Altomare (PI of the research project) through some communications including some workshops. Dr. Altomare hired a composite-modelling approach, consisting of both physical and numerical modelling. Physical model tests were carried out in two different wave flume facilities in UPC, meanwhile the numerical modelling using mesh-free DualSPHysics model was performed. On top, the EPR data-driven technique was also used to find new correlations between wave impacts and overtopping flows. As a result, Dr. Altomare published 14 articles (8 are collaboration with FHR) – at the moment of mid-March 2021. Through this following up project, FHR obtained further knowledge on wave overtopping processes, more specifically directional spreading effect on coastal dikes in shallow foreshores and overtopping flow characteristics on a dike in shallow foreshores. These knowledge are very relevant to the work of FHR, especially for the risk assessment of the coasts.
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Offshore wave boundary conditions often consist of energy density spectra being readily available (e.g. offshore wave buoys) or idealized energy density spectra of which the parameters are reported (e.g. in the Hydraulic Boundary Condition book, De Roo et al., 2016). In numerical modelling, an infinite number of surface elevation time series can be generated out of one energy density spectrum by linearly superposing the spectral wave components, of which the phases are assumed to be randomly distributed. To create randomly varying phase components, an input seed number is needed. By varying this seed number for every simulation, a different surface elevation time series, i.e. different wave train, will be created. The number of waves overtopping a structure is governed by the number of large wave heights in the wave train and the specific sequence of waves arriving at the structure. Hence, random wave trains resulting from the same energy density spectrum, lead possibly to different volumes of waves that overtop and introduce variability in the numerically estimated wave overtopping discharge. To assess this variability in wave overtopping, 500 simulations were carried out for every case. In total, 18 cases were identified by categorizing the Flemish coastline into 6 generalized bathymetric configurations, varying in cross shore profile, in foreshore length, in presence of a steeper part in its slope closer to the dike and ending in a dike, have a 1:2 slope and 3 different crest levels. Given that wave overtopping discharge is accepted to be normally distributed, its mean result and the variability around this value can be assessed by its relative error. The higher the mean wave overtopping discharge, the lower the relative error becomes (power law relation). Indeed, the higher the freeboard, the smaller the probability of overtopping, and hence, the more wave overtopping depends on the individual wave characteristics in the surface elevation time series. Translating this fitted relation to a confidence band around the mean indicates that 68.3% of the wave overtopping values are captured within ± 1 standard deviation around the mean. The upper confidence limit, generally used for design and assessment purposes, adds some safety to the mean result, and hence, the mean wave overtopping result needs to be increased by its associated standard deviation to account for seed number variability. In practice, it is not possible to carry out that amount of simulations to determine the wave overtopping discharge. Applying both a Monte Carlo and data sampling approach, the added uncertainty was quantified given that only a reduced sample of 1 to 20 wave overtopping estimates is used instead of 500. As from a sample size of 8, the added accuracy gained by increasing the sample size becomes insignificant compared to the calculation effort of doing extra simulations. Therefore, a sample size of 8 is opted for. To conclude, wave overtopping discharge needs to be estimated by at least 8 SWASH 1D simulations. Their mean result is then the wave overtopping discharge on which for seed number selection and sample size uncertainty needs to be accounted for, in order to obtain a final numerical estimate of the wave overtopping discharge.
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