<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Bjørk, Anders A.</dc:creator>
  <dc:creator>Aagaard, S.</dc:creator>
  <dc:creator>Lütt, A.</dc:creator>
  <dc:creator>Khan, S. A.</dc:creator>
  <dc:creator>Box, J. E.</dc:creator>
  <dc:creator>Kjeldsen, K. K.</dc:creator>
  <dc:creator>Larsen, N. K.</dc:creator>
  <dc:creator>Korsgaard, N. J.</dc:creator>
  <dc:creator>Cappelen, J.</dc:creator>
  <dc:creator>Colgan, W. T.</dc:creator>
  <dc:creator>Machguth, Horst</dc:creator>
  <dc:creator>Andresen, C. S.</dc:creator>
  <dc:creator>Peings, Y.</dc:creator>
  <dc:creator>Kjær, K. H.</dc:creator>
  <dc:date>2017-12-18</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Glaciers and ice caps peripheral to the main Greenland Ice Sheet contribute markedly  to sea-level rise1,2,3. Their changes and variability, however, have been difficult to  quantify on multi-decadal timescales due to an absence of long-term data4. Here,  using historical aerial surveys, expedition photographs, spy satellite imagery and new  remote-sensing products, we map glacier length fluctuations of approximately 350  peripheral glaciers and ice caps in East and West Greenland since 1890. Peripheral  glaciers are found to have recently undergone a widespread and significant retreat at  rates of 12.2 m per year and 16.6 m per year in East and West Greenland,  respectively; these changes are exceeded in severity only by the early twentieth  century post-Little-Ice-Age retreat. Regional changes in ice volume, as reflected by  glacier length, are further shown to be related to changes in precipitation associated  with the North Atlantic Oscillation (NAO), with a distinct east–west asymmetry; positive  phases of the NAO increase accumulation, and thereby glacier growth, in the eastern  periphery, whereas opposite effects are observed in the western periphery. Thus, with  projected trends towards positive NAO in the future5,6, eastern peripheral glaciers  may remain relatively stable, while western peripheral glaciers will continue to  diminish.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/306574</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/306574/files/mac_cgp.pdf</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/306574/files/mac_cgp_sm.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1038/s41558-017-0029-1</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Nature Climate Change. - 2018, vol. 8, no. 1, p. 48–52</dc:source>
  <dc:subject>info:eu-repo/classification/udc/556</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Changes in Greenland’s peripheral glaciers linked to the North Atlantic Oscillation</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
