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dc.contributor.authorThiéblemont, Rémi
dc.contributor.authorLe Cozanne, Gonéri
dc.contributor.authorRohmer, Jérémy
dc.contributor.authorToimil Silva, Alexandra
dc.contributor.authorÁlvarez Cuesta, Moisés 
dc.contributor.authorLosada Rodríguez, Iñigo 
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2022-02-08T18:39:43Z
dc.date.available2022-02-08T18:39:43Z
dc.date.issued2021
dc.identifier.issn1561-8633
dc.identifier.issn1684-9981
dc.identifier.other690462es_ES
dc.identifier.urihttp://hdl.handle.net/10902/23904
dc.description.abstractABSTRACT:Global mean sea level rise and its acceleration are projected to aggravate coastal erosion over the 21st century, which constitutes a major challenge for coastal adaptation. Projections of shoreline retreat are highly uncertain, however, namely due to deeply uncertain mean sea level projections and the absence of consensus on a coastal impact model. An improved understanding and a better quantification of these sources of deep uncertainty are hence required to improve coastal risk management and inform adaptation decisions. In this work we present and apply a new extraprobabilistic framework to develop shoreline change projections of sandy coasts that allows consideration of intrinsic (or aleatory) and knowledge-based (or epistemic) uncertainties exhaustively and transparently. This framework builds upon an empirical shoreline change model to which we ascribe possibility functions to represent deeply uncertain variables. The model is applied to two local sites in Aquitaine (France) and Castellón (Spain). First, we validate the framework against historical shoreline observations and then develop shoreline change projections that account for possible (although unlikely) low-end and high-end mean sea level scenarios. Our high-end projections show for instance that shoreline retreats of up to 200m in Aquitaine and 130m in Castellón are plausible by 2100, while low-end projections revealed that 58 and 37m modest shoreline retreats, respectively, are also plausible. Such extended intervals of possible future shoreline changes reflect an ambiguity in the probabilistic description of shoreline change projections, which could be substantially reduced by better constraining sea level rise (SLR) projections and improving coastal impact models. We found for instance that if mean sea level by 2100 does not exceed 1m, the ambiguity can be reduced by more than 50%. This could be achieved through an ambitious climate mitigation policy and improved knowledge on ice sheets.es_ES
dc.description.sponsorshipThis research has been supported by the BRGM, IHCantabria and the ERA4CS-ECLISEA project (grant no. 690462).es_ES
dc.format.extent20 p.es_ES
dc.language.isoenges_ES
dc.publisherEuropean Geosciences Union (EGU) ; Copernicus Publications (editor comercial)es_ES
dc.rightsAttribution 4.0 Internationales_ES
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.sourceNatural hazards and earth system sciences 2021, 21, 7, 2257 - 2276es_ES
dc.titleDeep uncertainties in shoreline change projections: an extra-probabilistic approach applied to sandy beacheses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.5194/nhess-21-2257-2021es_ES
dc.rights.accessRightsopenAccesses_ES
dc.identifier.DOI10.5194/nhess-21-2257-2021
dc.type.versionpublishedVersiones_ES


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Attribution 4.0 InternationalExcepto si se señala otra cosa, la licencia del ítem se describe como Attribution 4.0 International