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Wave-driven storm impacts on Scotland's sedimentary barriers intensify with climate change

datacite.subject.sdg13:Ação Climática
datacite.subject.sdg14:Proteger a Vida Marinha
datacite.subject.sdg11:Cidades e Comunidades Sustentáveis
dc.contributor.authorHorsburgh, Nicola
dc.contributor.authorLoureiro, Carlos
dc.contributor.authorRennie, Alistair
dc.contributor.authorHurst, Martin
dc.contributor.authorNaylor, Larissa A.
dc.contributor.authorTyler, Andrew
dc.date.accessioned2026-09-28T15:08:48Z
dc.date.available2026-09-28T15:08:48Z
dc.date.issued2026-08-12
dc.description.abstractBeaches and dunes form vital natural barriers, protecting coastal communities from extreme sea levels. To support coastal management, a geomorphologically-informed understanding of how barriers may be impacted by storm-induced coastal hazards is essential. While storm wave runup can contribute significantly to local extreme sea levels and drive dramatic short- and near-term morphological change to sedimentary coasts, it remains only partly characterised in existing national and regional assessments. This study investigates wave-driven storm impacts at large spatial scales (100–1000 km), at a resolution sufficient to inform local decision making. Using higher resolution national and European datasets, established empirical parameterisations and a simplified barrier morphological evolution model, we predict extreme wave runup and storm impacts on Scotland's wavedominated sedimentary coasts, at 50 m alongshore resolution. We consider a synthetic storm comprised of 25- year return levels of tides and storm surge, and the 1% exceedance of wave height and period, and predict storm impacts for the present-day, mid- and end-century, under RCP4.5 and RCP8.5. Results show that wave runup contributes on average 38% to extreme sea levels, and over 50% in the most exposed locations under present conditions. Nationally, 416 km (65% of the assessed coast) experience barrier erosion during the synthetic storm event, while 72 km (11%) and 27 km (4%) undergo overwash and inundation, respectively. By 2100 the predicted length of inundated coast approximately doubles to 46 km (7%) under RCP4.5, and 59 km (9%) under RCP8.5. Results reveal strong sub-national variability in storm impacts, identifying clear hotspots with the potential for erosion-enhanced flooding.eng
dc.description.sponsorshipUID/0350/2020
dc.identifier.doi10.1016/j.geomorph.2026.110489
dc.identifier.issn0169-555X
dc.identifier.urihttp://hdl.handle.net/10400.1/29533
dc.language.isoeng
dc.peerreviewedyes
dc.publisherElsevier BV
dc.relationAquatic Research Infrastructure Network
dc.relation.ispartofGeomorphology
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subjectExtreme wave runup
dc.subjectStorm impacts
dc.subjectCoastal barriers
dc.subjectNational assessment
dc.subjectClimate change
dc.subjectGeospatial
dc.titleWave-driven storm impacts on Scotland's sedimentary barriers intensify with climate changeeng
dc.typejournal article
dspace.entity.typePublication
oaire.awardNumberLA/P/0069/2020
oaire.awardTitleAquatic Research Infrastructure Network
oaire.awardURIinfo:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/LA%2FP%2F0069%2F2020/PT
oaire.citation.startPage110489
oaire.citation.titleGeomorphology
oaire.citation.volume513
oaire.fundingStream6817 - DCRRNI ID
oaire.versionhttp://purl.org/coar/version/c_970fb48d4fbd8a85
person.familyNameLoureiro
person.givenNameCarlos
person.identifier453264
person.identifier.ciencia-id011D-31BD-C6B6
person.identifier.orcid0000-0003-3117-3492
person.identifier.ridU-9863-2018
person.identifier.scopus-author-id23667861200
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.nameFundação para a Ciência e a Tecnologia
relation.isAuthorOfPublication0da09945-415f-4574-a444-268a1c05b544
relation.isAuthorOfPublication.latestForDiscovery0da09945-415f-4574-a444-268a1c05b544
relation.isProjectOfPublication5af011f9-3888-449a-a18c-d08b59e87091
relation.isProjectOfPublication.latestForDiscovery5af011f9-3888-449a-a18c-d08b59e87091

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