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dc.rights.licenseopenen_US
dc.contributor.authorNICOLAE LERMA, Alexandre
dc.contributor.authorCASTELLE, Bruno
IDREF: 087596520
dc.contributor.authorMARIEU, Vincent
dc.contributor.authorROBINET, Arthur
dc.contributor.authorBULTEAU, Thomas
dc.contributor.authorBERNON, Nicolas
dc.contributor.authorMALLET, Cyril
dc.date.accessioned2022-11-08T14:50:54Z
dc.date.available2022-11-08T14:50:54Z
dc.date.issued2022-02
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/170228
dc.description.abstractEnLarge-scale coastal monitoring programs are challenging to maintain over time but are necessary to understand and further predict complex coastal evolution and resilience. The 230 km-long Aquitaine coast is a high-energy meso-macrotidal coast composed of beach-dune systems showing dramatic morphological changes at seasonal and interannual scales. This study investigates the alongshore variability in beach-dune response based on a unique 11-year dataset of 41 spaced transects surveyed yearly in spring. The dataset is completed by interspersed autumn LiDAR surveys for seasonal analysis. Several beach-dune morphological descriptors are developed, such as beach-dune volume, beach width and different shoreline proxies delimiting the intertidal zone, the beach face and the dune face. The Aquitaine beach-dune system is characterised by a north-south gradient, from chronically eroding dunes backing low-elevation dissipative beaches in the north, to slowly accreting dunes backing wide beaches in the south, through a range of intermediate beach-dune states. Time- and spatially-averaged shoreline (dune foot position) trend is −0.5 m/year (erosion), with local variations ranging from −5.9 m/year to +2.1 m/year. During the 2013–2014 winter widespread erosion was observed, with the shoreline eroding by 13 m and 8 m on average along the Gironde and Landes coasts, respectively. This dataset provides insight into the timing, magnitude and spatial variability of beach-dune recovery from the outstandingly erosive 2013–2014 winter. We also show that local beach-dune volume is a good proxy for long-term shoreline trend. It is advocated that such large-scale coastal monitoring by means of single beach profiles spaced and distributed along 10–100 km of coast is a cheap and efficient approach to address coastal changes at regional scale, which can bring complementary information to aerial photographs interpretation to determine long-term shoreline evolution trend and thus contribute to support sustainable coastal management and planning.
dc.language.isoENen_US
dc.subject.enBeach profile
dc.subject.enCoastal dune
dc.subject.enErosion
dc.subject.enLong-term trend
dc.subject.enRecovery
dc.subject.enRegional variability
dc.title.enDecadal beach-dune profile monitoring along a 230-km high-energy sandy coast: Aquitaine, southwest France
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.apgeog.2022.102645en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalApplied Geographyen_US
bordeaux.volume139en_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
hal.identifierhal-03831762
hal.version1
hal.exportfalse
dc.rights.ccPas de Licence CCen_US
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