<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-04-17T03:48:11Z</responseDate><request verb="GetRecord" identifier="oai:www.recercat.cat:2117/100636" metadataPrefix="oai_dc">https://recercat.cat/oai/request</request><GetRecord><record><header><identifier>oai:recercat.cat:2117/100636</identifier><datestamp>2026-01-14T07:50:03Z</datestamp><setSpec>com_2072_1033</setSpec><setSpec>col_2072_452950</setSpec></header><metadata><oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
   <dc:title>Modelling bedforms on the continental shelf</dc:title>
   <dc:creator>Calvete Manrique, Daniel</dc:creator>
   <dc:contributor>Universitat Politècnica de Catalunya. Departament de Física</dc:contributor>
   <dc:contributor>Universitat Politècnica de Catalunya. DF - Dinàmica No Lineal de Fluids</dc:contributor>
   <dc:subject>Àrees temàtiques de la UPC::Física</dc:subject>
   <dc:subject>Continental shelf</dc:subject>
   <dc:subject>Tides</dc:subject>
   <dc:subject>morphodynamic modelling</dc:subject>
   <dc:subject>continental shelf</dc:subject>
   <dc:subject>tidal sand waves</dc:subject>
   <dc:subject>tidal sand banks</dc:subject>
   <dc:subject>long bed waves</dc:subject>
   <dc:subject>shoreface-connected ridges</dc:subject>
   <dc:subject>Plataforma continental</dc:subject>
   <dc:subject>Marees</dc:subject>
   <dc:description>A number of morphodynamic models have been developed to simulate   the dynamics of large-scale bedform patterns on the continental shelf. Most of the models are based on linear stability analysis and, therefore, only describe the characteristics of the bedforms at their formation. Apart from studying the principal formation mechanism, the models have take into account various processes (three dimensional flows, sediment sorting, wave stirring, different tidal constituents, etc) to describe the characteristics of the bedforms at specific locations. Exploration of the finite amplitude regime have also been made with simplified models. Future model developments are needed to explore long-term dynamics.</dc:description>
   <dc:description>Postprint (author's final draft)</dc:description>
   <dc:date>2017</dc:date>
   <dc:type>Part of book or chapter of book</dc:type>
   <dc:identifier>Calvete, D. Modelling bedforms on the continental shelf. A: "Atlas of bedforms in the Western Mediterranean". Springer International Publishing, 2017, p. 19-24.</dc:identifier>
   <dc:identifier>978-3-319-33938-2</dc:identifier>
   <dc:identifier>https://hdl.handle.net/2117/100636</dc:identifier>
   <dc:identifier>10.1007/978-3-319-33940-5</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>http://link.springer.com/book/10.1007/978-3-319-33940-5</dc:relation>
   <dc:rights>http://creativecommons.org/licenses/by-nc-nd/3.0/es/</dc:rights>
   <dc:rights>Restricted access - publisher's policy</dc:rights>
   <dc:format>6 p.</dc:format>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Springer International Publishing</dc:publisher>
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