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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCABEZAS RABADAN, Carlos
dc.contributor.authorPARDO-PASCUAL, J.E.
dc.contributor.authorPALOMAR-VÁZQUEZ, J.
dc.contributor.authorROCH-TALENS, A.
dc.contributor.authorGUILLÉN, J.
dc.date.accessioned2025-04-25T12:43:41Z
dc.date.available2025-04-25T12:43:41Z
dc.date.issued2024-03
dc.identifier.issn0378-3839en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/206451
dc.description.abstractEnStorms and extremely energetic events may significantly impact the form and structure of beaches, and so cause erosive processes and coastal damages. Efficient management actions require an up-to-date and accurate knowledge of beach morphological changes, with the shoreline position being a good indicator of such changes. This work proposes the use of the open-source Shoreline Analysis and Extraction Tool (SAET) software for the definition of satellite-derived shorelines (SDSs) from L8 and Sentinel-2 imagery to reveal the shoreline position changes at the beaches of the Ebro Delta, NE Spain. Spatial-temporal models (STMs) of shoreline changes enable a characterisation of how the beaches responded to the storms of 2020. In conjunction with wave data, STMs enable an analysis of the erosive response to storm events, as well as a monitoring of subsequent beach recovery in the short and medium term (<1 year). Results show how Storm Gloria (January 2020, Hs max = 7.62 m) acted as a disruptive event and shifting point in the shoreline trend. As a response to that storm, major erosive processes occurred along the delta that caused an average shoreline retreat of 47 m. A progressive recovery during the spring and summer was mainly associated with periods of low wave energy. Nevertheless, by the end of the year a complete recovery had been achieved for about half of the coast, while the other half showed an average erosion of more than 10 m when compared to the pre-storm situation. Both the erosive and the recovery processes took place unevenly on different sections of the coast, probably dependent on factors such as the orientation of the beach and the pattern of longitudinal sediment transport along the coast.
dc.language.isoENen_US
dc.subject.enSubpixel shoreline extraction
dc.subject.enCoastal storm monitoring
dc.subject.enBeach morphological characterisation
dc.subject.enSAET
dc.subject.enSentinel-2
dc.subject.enLandsat
dc.subject.enErosion and recovery
dc.title.enSatellite observations of storm erosion and recovery of the Ebro Delta coastline, NE Spain
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.coastaleng.2023.104451en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalCoastal Engineeringen_US
bordeaux.page104451en_US
bordeaux.volume188en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcecrossref
hal.identifierhal-05047083
hal.version1
hal.date.transferred2025-04-25T12:43:43Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcecrossref
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&amp;rft_val_fmt=info:ofi/fmt:kev:mtx:journal&amp;rft.jtitle=Coastal%20Engineering&amp;rft.date=2024-03&amp;rft.volume=188&amp;rft.spage=104451&amp;rft.epage=104451&amp;rft.eissn=0378-3839&amp;rft.issn=0378-3839&amp;rft.au=CABEZAS%20RABADAN,%20Carlos&amp;PARDO-PASCUAL,%20J.E.&amp;PALOMAR-V%C3%81ZQUEZ,%20J.&amp;ROCH-TALENS,%20A.&amp;GUILL%C3%89N,%20J.&amp;rft.genre=article


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