Present and future flooding and erosion along the NW Spanish Mediterranean Coast

Coastal flooding and eros-ion caused by extreme events are the main factors responsible for beach hazards. This effect will be exacerbated by the sea level rise induced by climate change. The present work determines the vulnerability to erosion and flooding along 55 beaches grouped in different coas...

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Detalles Bibliográficos
Autores: Sánchez Artús, Xavier|||0000-0003-1478-1840, Gracia García, Vicente|||0000-0002-4628-426X, Espino Infantes, Manuel|||0000-0002-9026-3976, Sierra Pedrico, Juan Pablo|||0000-0003-0814-1134, Pinyol Guamis, Jordi, Sánchez-Arcilla Conejo, Agustín|||0000-0002-3450-6697
Tipo de recurso: artículo
Fecha de publicación:2023
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:2117/390484
Acceso en línea:https://hdl.handle.net/2117/390484
https://dx.doi.org/10.3389/fmars.2023.1125138
Access Level:acceso abierto
Palabra clave:Beach erosion
Climate change
XBeach
Fooding
Erosion
Sea level
Modeling
Sandy beaches
Platges -- Erosió
Àrees temàtiques de la UPC::Enginyeria civil::Enginyeria hidràulica, marítima i sanitària::Ports i costes
Descripción
Sumario:Coastal flooding and eros-ion caused by extreme events are the main factors responsible for beach hazards. This effect will be exacerbated by the sea level rise induced by climate change. The present work determines the vulnerability to erosion and flooding along 55 beaches grouped in different coastal archetypes, representative of the Catalan coast. The vulnerability assessment has been done through the numerical simulation of different combinations for projected waves and mean water levels under present conditions and the climate change scenarios RCP4.5 and RCP8.5 for the year 2100. A storm event approach has been used to determine coastal flooding and erosion with return periods of 50, 100, and 500 years using the XBeach numerical model. Results show that shoreline retreat is not the best proxy to characterize the erosion. The low-lying nature of the coast, the non-presence of well-developed berms, and the existence of river mouth and torrents govern the coastal flooding. The sea level rise appears to be a dominant variable in coastal hazards.