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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>2018-01-15T18:34:52Z</responseDate> <request identifier=oai:HAL:hal-00831573v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00831573v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:COMM</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:spi</setSpec> <setSpec>subject:phys</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:CEREGE</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:OSU-INSTITUT-PYTHEAS</setSpec> <setSpec>collection:MIO</setSpec> <setSpec>collection:UNIV-AMU</setSpec> <setSpec>collection:UNIV-TLN</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:PSL</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:CDF</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>WAVE SETUP AND WATERTABLE OVERHEIGHT IN THE CIGU SAND BARRIER (TAIWAN) DURING THE TALIM TROPICAL STORM</title> <creator>Sous, Damien</creator> <creator>Campmas, Lucie</creator> <creator>Meulé, Samuel</creator> <creator>Bouchette, Frederic</creator> <creator>Liou, Jying Li</creator> <creator>Rey, Vincent</creator> <creator>TOUBOUL, Julien</creator> <contributor>Institut méditerranéen d'océanologie (MIO) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Institut de recherche pour le développement [IRD] : UMR235 - Université de Toulon (UTLN) - Centre National de la Recherche Scientifique (CNRS)</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>thl ; Université du Québec</contributor> <description>International audience</description> <source>Coastal Dynamics 2013</source> <identifier>hal-00831573</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00831573</identifier> <source>https://hal.archives-ouvertes.fr/hal-00831573</source> <source>Coastal Dynamics 2013, Jun 2013, France</source> <language>en</language> <subject>[SDU.OCEAN] Sciences of the Universe [physics]/Ocean, Atmosphere</subject> <subject>[SPI.MECA.MEFL] Engineering Sciences [physics]/Mechanics [physics.med-ph]/Fluids mechanics [physics.class-ph]</subject> <subject>[PHYS.MECA.MEFL] Physics [physics]/Mechanics [physics]/Mechanics of the fluids [physics.class-ph]</subject> <type>info:eu-repo/semantics/conferenceObject</type> <type>Conference papers</type> <description lang=en>The present research work is a part of the KUNSHEN Franco-Taiwanese research project which aims at investigating the hydro/morphodynamics of barrier islands driven by typhoon events. This study focuses on the impact of the Talim tropical storm on the Wan-tzu-liao sand barrier (Taiwan) in terms of water level rising and watertable overheight. In-situ measurements are provided by a cross-shore network of pressure sensors extended from the intertidal zone to the top of the barrier. Extreme offshore wave conditions are encountered during Talim, with significant wave height greater than 10m at the storm peak. It is shown that measured setups are smaller than those predicted by usual empirical parameterization. Groundwater dynamics is strongly affected by the storm, with watertable overheight of the order of one meter under the barrier top. Watertable dynamics is influenced by waves, tides and rainfalls.</description> <date>2013-06-24</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>