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<title lang=en>Shoreline and upper beach dynamics under extreme events : the KUNSHEN experiment (Wan-tzu-liao barrier, Taiwan)</title>
<creator>Meulé, Samuel</creator>
<creator>CAMPMAS, Lucie</creator>
<creator>Bouchette, Frederic</creator>
<creator>Liou, Jying Li</creator>
<creator>Sabatier, F.</creator>
<creator>Sous, Damien</creator>
<creator>Sylaios, Georgios</creator>
<creator>Rey, Vincent</creator>
<creator>Wu, Y.C.</creator>
<creator>Lin, T.Y.</creator>
<creator>Hwung, H.-H.</creator>
<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>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>Risques ; 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) - 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>Laboratory of Ecological Engineering & Technology, Department of Environmental Engineering, University of Thrace ; Université du Québec</contributor>
<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>
<source>ISSN: 1760-8716</source>
<source>Revue Paralia</source>
<publisher>Editions Paralia CFL</publisher>
<identifier>hal-00854411</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00854411</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00854411</source>
<source>Revue Paralia, Editions Paralia CFL, 2012, XII emes Journées Nationales Génie Cotier - Génie (Cherbourg, 12-14 juin 2012), pp.595-602. 〈10.5150/jngcgc.2012.034-M〉</source>
<identifier>DOI : 10.5150/jngcgc.2012.034-M</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.5150/jngcgc.2012.034-M</relation>
<language>en</language>
<subject lang=en>Extreme events</subject>
<subject lang=en>Submersion</subject>
<subject lang=en>Typhoon</subject>
<subject lang=en>Taiwan</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>Barrier island hydro-morphodynamics driven by typhoon events are the major concern of the project KUNSHEN (2011-2014). It aims at providing for a deep understanding of the peculiar dynamics of sand barriers where extreme events such as typhoons have a significant impact. We present the campaigns and the protocols achieved and planned in the project, on the Wan-tzu-liao sand barrier, Cigu Lagoon, Tainan, Taiwan, from October 2011 to January 2012, during the winter storm season and during summer 2012 during the typhoon season. A set of current profilers are deployed along a cross shore transect at 7, 4 and 2 meters deep. On the Wan-tzu-liao sand barrier, 3 columns of 3 pressiometers are deployed to survey the submersion. In the same time, morphological surveys are performed on the sand barrier with DGPS to analyse any change in the shoreline position, the beach slope, and the dynamics of sand beach features. A very preliminary analysis on these on-going field surveys suggests that the word "extreme" refers more to the consequence of the forcing on the sand barrier than the intensity of the forcing itself. The strategy developed in this first step will be refined to survey the next typhoon season, from May 2012 to October 2012.</description>
<date>2012-07-26</date>
</dc>
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