Journal article Open Access

Modeling the evolution of the Antarctic ice sheet in the last 200ky

F. Baratelli; Mauro Giudici; Cecilia Balconi; Chiara Vassena


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  <identifier identifierType="URL">https://www.openaccessrepository.it/record/88283</identifier>
  <creators>
    <creator>
      <creatorName>F. Baratelli</creatorName>
    </creator>
    <creator>
      <creatorName>Mauro Giudici</creatorName>
    </creator>
    <creator>
      <creatorName>Cecilia Balconi</creatorName>
    </creator>
    <creator>
      <creatorName>Chiara Vassena</creatorName>
    </creator>
  </creators>
  <titles>
    <title>Modeling the evolution of the Antarctic ice sheet in the last 200ky</title>
  </titles>
  <publisher>INFN Open Access Repository</publisher>
  <publicationYear>2010</publicationYear>
  <subjects>
    <subject>NEANIAS Atmospheric Research Community</subject>
    <subject>General Medicine</subject>
  </subjects>
  <dates>
    <date dateType="Issued">2010-01-01</date>
  </dates>
  <language>en</language>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://www.openaccessrepository.it/record/88283</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1016/j.sbspro.2010.05.138</relatedIdentifier>
    <relatedIdentifier relatedIdentifierType="URL" relationType="IsPartOf">https://www.openaccessrepository.it/communities/itmirror</relatedIdentifier>
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  <rightsList>
    <rights rightsURI="https://creativecommons.org/licenses/by-nc-nd/4.0/">Creative Commons Attribution-NonCommercial-NoDerivatives</rights>
    <rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights>
  </rightsList>
  <descriptions>
    <description descriptionType="Abstract">Abstract The evolution of the Antarctic ice sheet for the last 200 ky is simulated with a finite difference thermomechanical model based on the shallow ice approximation. The model depends on the surface temperature, the ice accumulation rate, the geothermal heat flux and the basal sliding coefficient, which are estimated with large uncertainty. Therefore a sensitivity analysis is applied to assess the most critical parameters.</description>
  </descriptions>
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