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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T18:37:35Z</responseDate> <request identifier=oai:HAL:hal-00767593v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00767593v1</identifier> <datestamp>2018-01-15</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-ROUEN</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:UNIV-AMU</setSpec> <setSpec>collection:UNIV-PERP</setSpec> <setSpec>collection:UMR6143M2C</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:COMUE-NORMANDIE</setSpec> <setSpec>collection:DYNALIT</setSpec> <setSpec>collection:PSL</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:CDF</setSpec> <setSpec>collection:CEREGE</setSpec> <setSpec>collection:OSU-INSTITUT-PYTHEAS</setSpec> <setSpec>collection:UNIV-CAEN</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Hydrodynamics over a microtidal double crescentic barred beach in low energetic conditions (Leucate Beach, France)</title> <creator>Ferrer, P.</creator> <creator>Certain, R.</creator> <creator>Adloff, F.</creator> <creator>Bouchette, Frederic</creator> <creator>Barusseau, J. -P.</creator> <creator>Meule, S.</creator> <creator>Robin, N.</creator> <contributor>Morphodynamique Continentale et Côtière (M2C) ; Centre National de la Recherche Scientifique (CNRS) - Université de Rouen Normandie (URN) ; Normandie Université (NU) - Normandie Université (NU) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Caen Normandie (UNICAEN) ; Normandie Université (NU)</contributor> <contributor>Université de Perpignan Via Domitia (UPVD)</contributor> <contributor>Max Planck Institute for Meteorology (MPI-M)</contributor> <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>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> <source>ISSN: 0749-0208</source> <source>EISSN: 1551-5036</source> <source>Journal of Coastal Research</source> <source>Special Issue 64 - ICS 2011 Proceedings (Szczecin, Poland) [Furmanczyk, Giza, & Terefenko]</source> <source>ICS 2011 - 11th International Coastal Symposium</source> <coverage>Szczecin, Poland</coverage> <publisher>Coastal Education and Research Foundation</publisher> <identifier>hal-00767593</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00767593</identifier> <source>https://hal.archives-ouvertes.fr/hal-00767593</source> <source>Journal of Coastal Research, Coastal Education and Research Foundation, 2011, SI64, pp.2032-2036</source> <language>en</language> <subject lang=en>Wave</subject> <subject lang=en>Current</subject> <subject lang=en>Rhythmic Bar and Beach</subject> <subject lang=en>nearshore zone</subject> <subject lang=en>current profiles</subject> <subject>[SDU.OCEAN] Sciences of the Universe [physics]/Ocean, Atmosphere</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>The south part nearshore zone of the Gulf of Lions coast (Mediterranean Sea) is characterized by a double crescentic sandbar system. During the winter 2007, a campaign of intensive hydrodynamical measurements (current profiles) was realized. During this campaign, based mainly on ADCPs, the maximal recorded wave height was 1.5 m. Four events were observed; two of those had northern incidence, one with southern incidence and a last one with frontal incidence. This paper proposes 3D hydrodynamical circulation maps over this microtidal bar system. The currents described reveals rip, bed-return and longshore currents strongly influenced by the wind-waves forcing and the bathymetry. At the apex of the oblique incidence events, the longshore component is the most important. The breaker zone is only located over the inner bar. During storm waning conditions, the cross-shore currents appear over the trough of the outer bar. The hydrodynamic circulation is then compared with other observations made in the literature.</description> <date>2011</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>