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  <identifier identifierType="DOI">10.18453/rosdok_id00003533</identifier>
  <creators>
    <creator>
      <creatorName nameType="Personal">Scheibe, Ludwig</creatorName>
      <givenName>Ludwig</givenName>
      <familyName>Scheibe</familyName>
      <nameIdentifier nameIdentifierScheme="GND" schemeURI="http://d-nb.info/gnd/">http://d-nb.info/gnd/1253176477</nameIdentifier>
    </creator>
  </creators>
  <titles>
    <title>Thermal evolution models for Uranus and Neptune</title>
  </titles>
  <publisher>Universität Rostock</publisher>
  <publicationYear>2021</publicationYear>
  <resourceType resourceTypeGeneral="Text" />
  <subjects>
    <subject xml:lang="en" schemeURI="http://dewey.info/" subjectScheme="dewey">530 Physics</subject>
  </subjects>
  <dates>
    <date dateType="Created">2021</date>
  </dates>
  <language>en</language>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="PURL">http://purl.uni-rostock.de/rosdok/id00003533</alternateIdentifier>
    <alternateIdentifier alternateIdentifierType="URN">urn:nbn:de:gbv:28-rosdok_id00003533-9</alternateIdentifier>
  </alternateIdentifiers>
  <descriptions>
    <description descriptionType="Abstract">Uranus and Neptune (U&amp;N) have highly different intrinsic heat fluxes. Here, the principles behind a new computer code for calculating numerical structure and evolution models of planets are presented, and with this program the thermal evolution of U&amp;N is investigated using up-to-date equation of state data. Particularly, it is shown that the assumption of a thermal boundary layer in the planet's envelope, trapping part of its heat in the deep interior, impacts the planet's cooling drastically and thus allows for an explanation of U&amp;N's heat fluxes within the same framework.</description>
  </descriptions>
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