Benchmarking of numerical models for wave overtopping at dikes with shallow mildly sloping foreshores: Accuracy versus speed

Practitioners often employ diverse, though not always thoroughly validated, numerical models to directly or indirectly estimate wave overtopping (q) at sloping structures. These models, broadly classified as either phase- resolving or phase-averaged, each have strengths and limitations owing to the...

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Detalles Bibliográficos
Autores: Lashley, Chris H., Zanuttigh, Barbara, Bricker, Jeremy, Van der Meer, Jentsje, Altomare, Corrado|||0000-0001-8817-0431, Suzuki, T., Roeber, Volker, Oosterlo, Patrick
Tipo de recurso: artículo
Fecha de publicación:2020
País:España
Institución:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/340820
Acceso en línea:https://hdl.handle.net/2117/340820
https://dx.doi.org/10.1016/j.envsoft.2020.104740
Access Level:acceso abierto
Palabra clave:Ocean waves
Infragravity wave
openFOAM
BOSZ
XBeach
SWASH
SWAN
Onades
Descripción
Sumario:Practitioners often employ diverse, though not always thoroughly validated, numerical models to directly or indirectly estimate wave overtopping (q) at sloping structures. These models, broadly classified as either phase- resolving or phase-averaged, each have strengths and limitations owing to the physical schematization of pro-cesses within them. Models which resolve the vertical flow structure or the full wave spectrum (i.e. sea-swell (SS) and infragravity (IG) waves) are considered more accurate, but more computationally demanding than those with approximations. Here, we assess the speed-accuracy trade-off of six well-known models for estimating q, under shallow foreshore conditions. The results demonstrate that: i) q is underestimated by an order of magnitude when IG waves are neglected; ii) using more computationally-demanding models does not guarantee improved accuracy; and iii) with empirical corrections to incorporate IG waves, phase-averaged models like SWAN can perform on par, if not better than, phase-resolving models but with far less computational effort.