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<datestamp>2018-01-11</datestamp>
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<title lang=en>Upper beach reconstruction patternsafter moderate storm events</title>
<creator>CAMPMAS, Lucie</creator>
<creator>Bouchette, Frederic</creator>
<creator>Liou, Jying Li</creator>
<creator>Brambilla, Elena</creator>
<creator>Meulé, Samuel</creator>
<creator>Sylaios, Georgios</creator>
<creator>Sabatier, F.</creator>
<creator>Certain, R.</creator>
<creator>Robin, N.</creator>
<creator>Hwung, H.</creator>
<contributor>Risques ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>thl ; Université du Québec</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratory of Ecological Engineering & Technology, Department of Environmental Engineering, University of Thrace ; Université du Québec</contributor>
<contributor>Centre de formation et de recherche sur l'environnement marin (CEFREM) ; Université de Perpignan Via Domitia (UPVD) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<source>ISSN: 1760-8716</source>
<source>Revue Paralia</source>
<publisher>Editions Paralia CFL</publisher>
<identifier>hal-00854402</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00854402</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00854402</source>
<source>Revue Paralia, Editions Paralia CFL, 2012, XII emes Journées Nationales Génie Cotier - Génie (Cherbourg, 12-14 juin 2012), pp.233-240. 〈10.5150/jngcgc.2012.023-C〉</source>
<identifier>DOI : 10.5150/jngcgc.2012.023-C</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.5150/jngcgc.2012.023-C</relation>
<language>en</language>
<subject lang=en>Shoreline</subject>
<subject lang=en>Swash zone</subject>
<subject lang=en>Morphological patterns</subject>
<subject lang=en>Beach reconstruction</subject>
<subject>[SDU.STU.OC] Sciences of the Universe [physics]/Earth Sciences/Oceanography</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The wave-dominated beach barrier of Villeneuve-Lès-Maguelone extends between Palavas and Frontignan (Gul f of Lions, northernmost Me diterranean Sea), along a slightly natural sandy protected area char acterized by typical and well-expressed morphologies. In the nearshore, the sea bottom shows one or two approximately rectilinear sand bars. In 2010-2011, we pe rformed a 6 month-long monitoring (autumn 2010/late spring 2011) of a 500 meter-long se gment along this sand barrier. We used RTK D-GPS offering centimeter resolution to acquire sets of elevation data on the beach and the upper shoreface. The study is innovative because a full morphologic monitoring was performed each time the wave/ wind conditions changed significantly. These changes were tracked in real-time thanks to a set of hydrodynamic equipments deployed at sea, including well-known DREAL buoys. We identify from well- documented data: (1) a beach reconstruction cycle at the shorelin e after a moderate storm event (wave height at 3-4 m) and (2) how a sand bar in the nearshore migrates to the shoreline and drives the shoreline shift.</description>
<date>2012-07-26</date>
</dc>
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