{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,4]],"date-time":"2026-03-04T15:58:27Z","timestamp":1772639907617,"version":"3.50.1"},"publisher-location":"Cham","reference-count":10,"publisher":"Springer Nature Switzerland","isbn-type":[{"value":"9783032154729","type":"print"},{"value":"9783032154736","type":"electronic"}],"license":[{"start":{"date-parts":[[2026,1,1]],"date-time":"2026-01-01T00:00:00Z","timestamp":1767225600000},"content-version":"tdm","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0"},{"start":{"date-parts":[[2026,3,5]],"date-time":"2026-03-05T00:00:00Z","timestamp":1772668800000},"content-version":"vor","delay-in-days":63,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0"}],"content-domain":{"domain":["link.springer.com"],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[2026]]},"abstract":"<jats:title>Abstract<\/jats:title>\n                  <jats:p>Along wave-dominated sedimentary coasts, risks posed by chronic coastal erosion and rising sea levels during this century have received much attention. However, extreme wave runup during large storms are still poorly characterised at large spatial scales, and can contribute significantly to coastal flooding and erosion. This creates an important challenge for coastal management and adaptation planning. This work presents a national-scale storm impact assessment for Scotland\u2019s wave-dominated sand and gravel coasts. It uses readily available national and European datasets to model extreme total water levels that include storm wave runup, tides, storm surge and changes in mean sea level. Future impacts are assessed by integrating likely climate-driven changes to storm forcing and coastal morphology. Outputs estimate the likely storm impact regime at 50\u00a0m alongshore transects in Scotland\u2019s natural sand and gravel coasts for the present day, 2050 and 2100, considering climate change scenarios RCP4.5 and RCP8.5. Results indicate 65%, 11% and 4% of transects currently experience collision, overwash and inundation as the most severe storm impact. Towards 2100, transects in overwash and inundation increase to 20% (22%) for RCP4.5 (RCP8.5), but local increases vary considerably between coastal cells. This study contributes to a strategic, national scale understanding of coastal risk that supports the spatial prioritisation of areas in need of proactive adaptation solutions.<\/jats:p>","DOI":"10.1007\/978-3-032-15473-6_49","type":"book-chapter","created":{"date-parts":[[2026,3,4]],"date-time":"2026-03-04T10:31:13Z","timestamp":1772620273000},"page":"310-316","update-policy":"https:\/\/doi.org\/10.1007\/springer_crossmark_policy","source":"Crossref","is-referenced-by-count":0,"title":["Storm Impact Assessment for Scotland\u2019s Wave-Dominated Sedimentary Coasts"],"prefix":"10.1007","author":[{"given":"Nicola","family":"Horsburgh","sequence":"first","affiliation":[]},{"given":"Carlos","family":"Loureiro","sequence":"additional","affiliation":[]},{"given":"Martin","family":"Hurst","sequence":"additional","affiliation":[]},{"given":"Alistair","family":"Rennie","sequence":"additional","affiliation":[]},{"given":"Andrew","family":"Tyler","sequence":"additional","affiliation":[]}],"member":"297","published-online":{"date-parts":[[2026,3,5]]},"reference":[{"key":"49_CR1","doi-asserted-by":"publisher","DOI":"10.1017\/cft.2023.3","volume":"1","author":"L Reimann","year":"2023","unstructured":"Reimann L, Vafeidis AT, Honsel LE (2023) Population development as a driver of coastal risk: current trends and future pathways. Cambridge Prisms Coast. Futures 1:e14","journal-title":"Cambridge Prisms Coast. Futures"},{"issue":"1","key":"49_CR2","doi-asserted-by":"publisher","first-page":"12876","DOI":"10.1038\/s41598-018-30904-w","volume":"8","author":"L Mentaschi","year":"2018","unstructured":"Mentaschi L, Vousdoukas MI, Pekel JF et al (2018) Global long-term observations of coastal erosion and accretion. Sci Rep 8(1):12876","journal-title":"Sci Rep"},{"issue":"2","key":"49_CR3","doi-asserted-by":"publisher","DOI":"10.1088\/1748-9326\/acb504","volume":"18","author":"S Jevrejeva","year":"2023","unstructured":"Jevrejeva S, Williams J, Vousdoukas MI et al (2023) Future sea level rise dominates changes in worst case extreme sea levels along the global coastline by 2100. 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