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  <identifier identifierType="DOI">10.18453/rosdok_id00001450</identifier>
  <creators>
    <creator>
      <creatorName nameType="Personal">Becherer, Johannes</creatorName>
      <givenName>Johannes</givenName>
      <familyName>Becherer</familyName>
      <nameIdentifier nameIdentifierScheme="GND" schemeURI="http://d-nb.info/gnd/">http://d-nb.info/gnd/1062851544</nameIdentifier>
    </creator>
  </creators>
  <titles>
    <title>Estuarine circulation in well-mixed tidal inlets</title>
    <title>Ästuarine Zirkulation in gut durchmischten Gezeitenkanälen</title>
  </titles>
  <publisher>Universität Rostock</publisher>
  <publicationYear>2014</publicationYear>
  <resourceType resourceTypeGeneral="Text" />
  <subjects>
    <subject xml:lang="en" schemeURI="http://dewey.info/" subjectScheme="dewey">550 Earth sciences</subject>
    <subject xml:lang="en" schemeURI="http://dewey.info/" subjectScheme="dewey">530 Physics</subject>
  </subjects>
  <dates>
    <date dateType="Created">2014</date>
  </dates>
  <language>en</language>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="PURL">http://purl.uni-rostock.de/rosdok/id00001450</alternateIdentifier>
    <alternateIdentifier alternateIdentifierType="URN">urn:nbn:de:gbv:28-diss2014-0202-8</alternateIdentifier>
  </alternateIdentifiers>
  <descriptions>
    <description descriptionType="Abstract">Estuarine dynamics in tidal inlets is studied based on data of two measurement campaigns in the German Wadden Sea. We present the first direct observations of tidal straining in the Wadden Sea. We also observe asymmetric lateral circulation, which is generated by a systematic interplay of horizontal density gradients and centrifugal forcing. This process is found to be  responsible for residual estuarine exchange flow. Finally, an idealized model is developed to study the relevance of this process for other systems.</description>
  </descriptions>
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