<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>Strozzi, Tazio</dc:creator>
  <dc:creator>Caduff, Rafael</dc:creator>
  <dc:creator>Jones, Nina</dc:creator>
  <dc:creator>Barboux, Chloé</dc:creator>
  <dc:creator>Delaloye, Reynald</dc:creator>
  <dc:creator>Bodin, Xavier</dc:creator>
  <dc:creator>Kääb, Andreas</dc:creator>
  <dc:creator>Mätzler, Eva</dc:creator>
  <dc:creator>Schrott, Lothar</dc:creator>
  <dc:date>2020</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Active rock glaciers represent the best visual expression of mountain  permafrost that can be mapped and monitored directly using remotely sensed  data. Active rock glaciers are bodies that consist of a perennially frozen ice/rock  mixture and express a distinct flow-like morphology indicating downslope  permafrost creep movement. Annual rates of motion have ranged from a few  millimeters to several meters per year, varying within the annual cycle, from  year to year, as well as at the decennial time scale. During the last decade, in  situ observations in the European Alps have shown that active rock glaciers are  responding almost synchronously to inter-annual and decennial changes in  ground temperature, suggesting that the relative changes of their kinematics are  a general indicator of the evolution of mountain permafrost conditions. Here, we  used satellite radar interferometry (InSAR) to monitor the rate of motion of  various active rock glaciers in the Swiss Alps, Qeqertarsuaq (Western  Greenland), and the semiarid Andes of South America. Velocity time series  computed with Sentinel-1 SAR images, regularly acquired since 2014, every six  days over Europe and Greenland and every 12 days over the Andes, show  annual fluctuations, with higher velocities at the end of the summer. A JERS-1  image pair of 1996 and stacks of very high-resolution SAR images from  TerraSAR-X and Cosmo-SkyMed from 2008 to 2017 were analyzed using  InSAR and offset tracking over the Western Swiss Alps in order to extend the  main observation period of our study. A quantitative assessment of the accuracy  of InSAR and offset tracking was performed by comparison with in situ  methods. Our results for the three different study regions demonstrate that  Sentinel-1 InSAR can complement worldwide in situ measurements of active  rock glacier kinematics</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/unifr/documents/308385</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308385/files/del_mrg.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.3390/rs12030559</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Remote Sensing. - 2020, vol. 12, no. 3, p. 559</dc:source>
  <dc:subject>info:eu-repo/classification/udc/55</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Monitoring rock glacier kinematics with satellite synthetic aperture radar</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
