<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>Kapitsa, Vassiliy</dc:creator>
  <dc:creator>Shahgedanova, Maria</dc:creator>
  <dc:creator>Machguth, Horst</dc:creator>
  <dc:creator>Severskiy, Igor</dc:creator>
  <dc:creator>Medeu, Akhmetkal</dc:creator>
  <dc:date>2017-10-24</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Changes in the abundance and area of mountain lakes in the Djungarskiy (Jetysu)  Alatau between 2002 and 2014 were investigated using Landsat imagery. The number  of lakes increased by 6.2 % from 599 to 636 with a growth rate of 0.51 % a−1. The  combined areas were 16.26 ± 0.85 to 17.35 ± 0.92 km2 respectively and the overall  change was within the uncertainty of measurements. Fifty lakes, whose potential  outburst can damage existing infrastructure, were identified. The glacier bed  topography version 2 (GlabTop2) model was applied to simulate ice thickness and  subglacial topography using glacier outlines for 2000 and SRTM DEM (Shuttle Radar  Topography Mission digital elevation model) as input data achieving realistic patterns  of ice thickness. A total of 513 overdeepenings in the modelled glacier beds,  presenting potential sites for the development of lakes, were identified with a  combined area of 14.7 km2. Morphometric parameters of the modelled  overdeepenings were close to those of the existing lakes. A comparison of locations  of the overdeepenings and newly formed lakes in the areas de-glacierized in 2000– 2014 showed that 67 % of the lakes developed at the sites of the overdeepenings.  The rates of increase in areas of new lakes correlated with areas of modelled  overdeepenings. Locations where hazardous lakes may develop in the future were  identified. The GlabTop2 approach is shown to be a useful tool in hazard management  providing data on the potential evolution of future lakes.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/306174</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/306174/files/mac_aer.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.5194/nhess-17-1837-2017</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Nat. Hazards Earth Syst. Sci.. - 2017, vol. 17, no. 10, p. 1837–1856</dc:source>
  <dc:subject>info:eu-repo/classification/udc/556</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Assessment of evolution and risks of glacier lake outbursts in the Djungarskiy Alatau, Central Asia, using Landsat imagery and glacier bed topography modelling</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
