Por favor, use este identificador para citar o enlazar este ítem: http://dspace.azti.es/handle/24689/1684
Ficheros en este ítem:
No hay ficheros asociados a este ítem.
Registro completo de metadatos
Campo DC Valor Lengua/Idioma
dc.contributor.authorde Santiago, Inaki-
dc.contributor.authorPlomaritis, T. A.-
dc.contributor.authorAvalos, D.-
dc.contributor.authorGarnier, Roland-
dc.contributor.authorAbalia, Aritz-
dc.contributor.authorEpelde, Irati-
dc.contributor.authorLiria, Pedro-
dc.date.accessioned2024-03-12T11:49:12Z-
dc.date.available2024-03-12T11:49:12Z-
dc.date.issued2024-
dc.identifierWOS:001140658900001-
dc.identifier.issn0048-9697-
dc.identifier.urihttp://dspace.azti.es/handle/24689/1684-
dc.description.abstractThis study compares the performance of different wave overtopping estimation models at urban beaches. The models selected for comparison are the Mase et al. (2013) and EurOtop parametric models and the XBeach process-based model in surfbeat and non-hydrostatic mode. Seven energetic storms are selected between 2015 and 2022 with offshore significant wave height ranging between 3 m and 8 m and peak period between 12 s and 20 s to perform the model comparison. The information required to run and validate the models (beach slope, shoreface shape, absence/presence of overtopping) was collected for each storm from coastal videometry. To account for the uncertainties derived from the incident waves randomness and the bathymetry shape when using the process-based model, a series of simulations with random seed boundary conditions were run over two different realistic profile shapes for each storm. The present study is a pilot study on the beach of Zarautz; however, it can be extended to other beaches of the Basque coast. Results indicate that while Mase et al. (2013) and EurOtop tend to reasonably predict the absence or presence of overtopping events, they tend to underestimate the hazard level at the beach of Zarautz. Additionally, the beach underwater profile shape can affect the process-based model performance at intermediate intensity storms and to a lesser extend during moderate storms. Finally, the hazard level at the beach of Zarautz varies significantly alongshore due to the configuration of the seawall, highlighting the need for local adaptation measures. Considering that there is no model that systematically performs better than others, it might be reasonable to use model assemble techniques to draw conclusions from a probabilistic perspective.-
dc.language.isoEnglish-
dc.publisherELSEVIER-
dc.subjectWave overtopping-
dc.subjectCoastal flooding-
dc.subjectModelling-
dc.subjectUrban beach-
dc.subjectProcess -based model-
dc.subjectParametric model-
dc.subjectEarly warning system-
dc.subjectBasque coast-
dc.subjectBAYESIAN NETWORK-
dc.subject2013/2014 WINTER-
dc.subjectIMPACT-
dc.subjectUNCERTAINTY-
dc.subjectVARIABILITY-
dc.subjectATLANTIC-
dc.subjectHAZARDS-
dc.subjectRISKS-
dc.subjectRUNUP-
dc.titleComparison of wave overtopping estimation models for urban beaches. Towards an early warning system on the Basque coast-
dc.typeArticle; Early Access-
dc.identifier.journalSCIENCE OF THE TOTAL ENVIRONMENT-
dc.format.volume912-
dc.contributor.funder(ERDF) through the Interreg V-A Spain-France-Andorra Programme (POCTEFA)-
dc.contributor.funderCRUNCH project [FEDER-UCA18-107062]-
dc.contributor.funderRegional Andalucian government [PID2019-109143RB-I00]-
dc.contributor.funderMinistry of Science and Inno-vation-
dc.contributor.funderEuropean Union-
dc.contributor.funderBasque Government Emergencies and Meteorology Directorate and Puertos del Estado [1192]-
dc.contributor.funderAZTI's Marine Research - European Commission under the Erasmus Mundus Joint Master's Degree Programme in Water and Coastal Management (WACOMA) [586596-EPP-1-2017-1-IT-EPPKA1-JMD-MOB]-
dc.identifier.e-issn1879-1026-
dc.identifier.doi10.1016/j.scitotenv.2023.168783-
Aparece en las tipos de publicación: Artículos científicos



Los ítems de DSpace están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.