Publicação
Wave-driven storm impacts on Scotland's sedimentary barriers intensify with climate change
| datacite.subject.sdg | 13:Ação Climática | |
| datacite.subject.sdg | 14:Proteger a Vida Marinha | |
| datacite.subject.sdg | 11:Cidades e Comunidades Sustentáveis | |
| dc.contributor.author | Horsburgh, Nicola | |
| dc.contributor.author | Loureiro, Carlos | |
| dc.contributor.author | Rennie, Alistair | |
| dc.contributor.author | Hurst, Martin | |
| dc.contributor.author | Naylor, Larissa A. | |
| dc.contributor.author | Tyler, Andrew | |
| dc.date.accessioned | 2026-09-28T15:08:48Z | |
| dc.date.available | 2026-09-28T15:08:48Z | |
| dc.date.issued | 2026-08-12 | |
| dc.description.abstract | Beaches 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.sponsorship | UID/0350/2020 | |
| dc.identifier.doi | 10.1016/j.geomorph.2026.110489 | |
| dc.identifier.issn | 0169-555X | |
| dc.identifier.uri | http://hdl.handle.net/10400.1/29533 | |
| dc.language.iso | eng | |
| dc.peerreviewed | yes | |
| dc.publisher | Elsevier BV | |
| dc.relation | Aquatic Research Infrastructure Network | |
| dc.relation.ispartof | Geomorphology | |
| dc.rights.uri | http://creativecommons.org/licenses/by/4.0/ | |
| dc.subject | Extreme wave runup | |
| dc.subject | Storm impacts | |
| dc.subject | Coastal barriers | |
| dc.subject | National assessment | |
| dc.subject | Climate change | |
| dc.subject | Geospatial | |
| dc.title | Wave-driven storm impacts on Scotland's sedimentary barriers intensify with climate change | eng |
| dc.type | journal article | |
| dspace.entity.type | Publication | |
| oaire.awardNumber | LA/P/0069/2020 | |
| oaire.awardTitle | Aquatic Research Infrastructure Network | |
| oaire.awardURI | info:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/LA%2FP%2F0069%2F2020/PT | |
| oaire.citation.startPage | 110489 | |
| oaire.citation.title | Geomorphology | |
| oaire.citation.volume | 513 | |
| oaire.fundingStream | 6817 - DCRRNI ID | |
| oaire.version | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |
| person.familyName | Loureiro | |
| person.givenName | Carlos | |
| person.identifier | 453264 | |
| person.identifier.ciencia-id | 011D-31BD-C6B6 | |
| person.identifier.orcid | 0000-0003-3117-3492 | |
| person.identifier.rid | U-9863-2018 | |
| person.identifier.scopus-author-id | 23667861200 | |
| project.funder.identifier | http://doi.org/10.13039/501100001871 | |
| project.funder.name | Fundação para a Ciência e a Tecnologia | |
| relation.isAuthorOfPublication | 0da09945-415f-4574-a444-268a1c05b544 | |
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