<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>Naegeli, Kathrin</dc:creator>
  <dc:creator>Lovell, Harold</dc:creator>
  <dc:creator>Zemp, Michael</dc:creator>
  <dc:creator>Benn, Douglas I.</dc:creator>
  <dc:date>2014</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">The routing and storage of meltwater and the configuration of drainage systems in glaciers exert a profound influence on glacier behaviour. However, little is known about the hydrological systems of cold glaciers, which form a significant proportion of the total glacier population in the climate sensitive region of the High Arctic. Using glacio-speleological techniques, we obtained direct access to explore and survey three conduit systems and one moulin within the tongue area of Tellbreen, a small cold-based valley glacier in central Spitsbergen. More than 600 m of conduits were surveyed and mapped in plan, profile and cross-section view to analyse the configuration of the drainage system. The investigations revealed that cold-based glaciers can exhibit a dendritic drainage network with supra-, en- and subglacial components formed most likely by cut-and-closure processes as well as surface-to-bed drainage via moulins. Furthermore, we observed that water is stored within the glacier and released gradually via subglacial conduits during the winter months, forming a large and active icing in the proglacial area. The presence of supra-, en- and subglacial components, the surface-to-bed moulin and the dendritic subglacial drainage network suggest that existing models and understanding of the hydrology of cold glaciers needs to be re-evaluated, mostly concerning the different possible pathways and processes that form the hydrological system.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://sonar.ch/global/documents/304135</dc:identifier>
  <dc:identifier>https://sonar.ch/documents/304135/files/nae_dsd.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/geoa.12059</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Geografiska Annaler: Series A, Physical Geography. - 2014, vol. 96, no. 4, p. 591–608</dc:source>
  <dc:subject xmlns:ns1="xml" ns1:lang="en">cold glaciers</dc:subject>
  <dc:subject xmlns:ns2="xml" ns2:lang="en">englacial subglacial conduit</dc:subject>
  <dc:subject xmlns:ns3="xml" ns3:lang="en">glacier hydrology</dc:subject>
  <dc:subject xmlns:ns4="xml" ns4:lang="en">glacio speleology</dc:subject>
  <dc:subject xmlns:ns5="xml" ns5:lang="en">icings</dc:subject>
  <dc:subject xmlns:ns6="xml" ns6:lang="en">Svalbard</dc:subject>
  <dc:subject>info:eu-repo/classification/udc/556</dc:subject>
  <dc:title xmlns:ns7="xml" ns7:lang="en">Dendritic subglacial drainage systems in cold glaciers formed by cut-and-closure processes</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
