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  <identifier identifierType="DOI">10.18453/rosdok_id00000938</identifier>
  <creators>
    <creator>
      <creatorName nameType="Personal">Knöpfel, Rahel</creatorName>
      <givenName>Rahel</givenName>
      <familyName>Knöpfel</familyName>
      <nameIdentifier nameIdentifierScheme="GND" schemeURI="http://d-nb.info/gnd/">http://d-nb.info/gnd/1018502785</nameIdentifier>
    </creator>
  </creators>
  <titles>
    <title>An Idealized Radiative Transfer Scheme for Use in an Atmospheric General Circulation Model From the Surface up to the Mesopause Region</title>
  </titles>
  <publisher>Universität Rostock</publisher>
  <publicationYear>2011</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">2011</date>
  </dates>
  <language>en</language>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="PURL">http://purl.uni-rostock.de/rosdok/id00000938</alternateIdentifier>
    <alternateIdentifier alternateIdentifierType="URN">urn:nbn:de:gbv:28-diss2011-0172-7</alternateIdentifier>
  </alternateIdentifiers>
  <descriptions>
    <description descriptionType="Abstract">The  main purpose of this work is to develop a new continuous radiation scheme of medium complexity for use in atmospheric general circulation models. For this purpose the  transfer equations  are solved continuously from the surface up to the lower thermosphere,  including  deviations from the gray limit and local thermodynamic equilibrium in the long-wave regime, as well as the complete surface energy budget. Applying the new radiation scheme in a mechanistic general circulation model  with prescribed concentrations of the radiatively active constituents shows quite reasonable results.</description>
  </descriptions>
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