<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>Rastner, P.</dc:creator>
  <dc:creator>Joerg, P.C.</dc:creator>
  <dc:creator>Huss, Matthias</dc:creator>
  <dc:creator>Zemp, Michael</dc:creator>
  <dc:date>2016-10-01</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Since the end of the Little Ice Age around 1850, glaciers in Europe have strongly  retreated. Thanks to early topographic surveys in Switzerland, accurate maps are  available, which enable us to trace glacier changes back in time. The earliest map for  all of Switzerland that is usable for a detailed analysis is the Dufour map from around  1850 with subsequent topographic maps on a ~ 20 year interval. Despite the large  public and scientific interest in glacier changes through time, this historic dataset has  not yet been fully utilized for topographic change assessment or visualization of  historic glacier extents. In this study, we use eleven historical topographic maps and  more recent digital datasets for the region of Zermatt to analyze geometric changes  (length, area and volume) of Findelengletscher as well as for creating animations of  glacier evolution through time for use in public communication. All maps were  georeferenced, the contour lines digitized, and digital elevation models (DEMs) created  and co-registered. Additional digital data like the SRTM X-band DEM and high  resolution laser scanning data were used to extend the analysis until 2010. Moreover,  one independent DEM from aerial photogrammetry was used for comparison. During  the period 1859–2010, Findelengletscher lost 3.5 km of its length (6.9 km in 2010),  4.42 ± 0.13 km² of its area (15.05 ± 0.45 km² in 2010) and 1.32 ± 0.52 km³ of its  volume. The average rate of thickness loss is 0.45 ± 0.042 m yr&lt;sup&gt;− 1&lt;/sup&gt; for  the 151 years period. Four periods with high thickness change from  − 0.56 m ± 0.28 yr&lt;sup&gt;− 1&lt;/sup&gt; (1859–1881), − 0.40 ± 0.08 m yr&lt;sup&gt;− 1&lt;/sup&gt;  (1937–1965), − 0.90 ± 0.31 m yr&lt;sup&gt;− 1&lt;/sup&gt; (1995–2000) and  − 1.18 ± 0.02 m yr&lt;sup&gt;− 1&lt;/sup&gt; (2000–2005) have been identified. Small positive  thickness changes were found for the periods 1890–1909 (+ 0.09 ± 0.46 m yr&lt;sup&gt; − 1&lt;/sup&gt;) and 1988–1995 (+ 0.05 ± 0.24 m yr&lt;sup&gt;− 1&lt;/sup&gt;). During its retreat with  intermittent periods of advance, the glacier separated into three parts. The above  changes are demonstrated through an animation (available from the supplementary  material), which has been created to inform the general public.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/305389</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/305389/files/hus_hav.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gloplacha.2016.07.005</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Global and Planetary Change. - 2016, vol. 145, p. 67–77</dc:source>
  <dc:subject>info:eu-repo/classification/udc/556</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Historical analysis and visualization of the retreat of Findelengletscher, Switzerland, 1859–2010</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
