<?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>2026-06-04T05:45:00Z</responseDate><request verb="GetRecord" identifier="oai:riuma.uma.es:10630/16056" metadataPrefix="rdf">https://riuma.uma.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:riuma.uma.es:10630/16056</identifier><datestamp>2026-02-03T12:11:44Z</datestamp><setSpec>com_10630_2254</setSpec><setSpec>col_10630_37959</setSpec></header><metadata><rdf:RDF xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:doc="http://www.lyncode.com/xoai" xmlns:ds="http://dspace.org/ds/elements/1.1/" xmlns:ow="http://www.ontoweb.org/ontology/1#" xmlns:rdf="http://www.openarchives.org/OAI/2.0/rdf/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/rdf/ http://www.openarchives.org/OAI/2.0/rdf.xsd">
   <ow:Publication rdf:about="oai:riuma.uma.es:10630/16056">
      <dc:title>Interaction flow bathymetry at tidal scale in the main sill of the Strait of Gibraltar</dc:title>
      <dc:creator>García-Lafuente, Jesús</dc:creator>
      <dc:creator>Sammartino, Simone</dc:creator>
      <dc:creator>Sánchez-Garrido, José Carlos</dc:creator>
      <dc:creator>Naranjo-Rosa, Cristina Belén</dc:creator>
      <dc:creator>Sánchez-Leal, Ricardo</dc:creator>
      <dc:subject>Hidrodinámica - Gibraltar (Estrecho)</dc:subject>
      <dc:description>Data collected in the north and south channels of the main sill of the Strait of&#xd;
Gibraltar (Camarinal sill) are used to investigate processes connected to the internal&#xd;
hydraulics of the exchange through the Strait at tidal frequencies. Observations strongly&#xd;
suggest the setting up of hydraulic jumps at both the western and eastern flank of the sill,&#xd;
the latter associated with the reversal of the Mediterranean undercurrent during spring&#xd;
tides. The northern site is more sensitive to processes triggered by the formation and&#xd;
release of the jump formed east of the sill during intense enough ebb tide cycles, which is&#xd;
thus better traced at this location; the southern site detects more neatly the fluctuations and&#xd;
footprints associated with the hydraulic jump regularly formed to the west of the sill&#xd;
during flood tides. A detailed inspection of the high resolution bathymetry of the area&#xd;
reveals the existence of two enclosed depressions at either side of the sill, almost certainly&#xd;
carved by the bottom flow over the millennia, whose shape and morphology are suggestive&#xd;
of this spatial differentiation.</dc:description>
      <dc:date>2018-06-28T11:05:07Z</dc:date>
      <dc:date>2018-06-28T11:05:07Z</dc:date>
      <dc:date>2018</dc:date>
      <dc:date>2018-06-28</dc:date>
      <dc:type>conference output</dc:type>
      <dc:identifier>https://hdl.handle.net/10630/16056</dc:identifier>
      <dc:language>eng</dc:language>
      <dc:relation>VI International Symposium on Marine Sciences</dc:relation>
      <dc:relation>Vigo (España)</dc:relation>
      <dc:relation>20 de Junio de 2018</dc:relation>
      <dc:rights>open access</dc:rights>
   </ow:Publication>
</rdf:RDF>
</metadata></record></GetRecord></OAI-PMH>