<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>He, Zhihua</dc:creator>
  <dc:creator>Unger-Shayesteh, Katy</dc:creator>
  <dc:creator>Vorogushyn, Sergiy</dc:creator>
  <dc:creator>Weise, Stephan M.</dc:creator>
  <dc:creator>Kalashnikov, Olga</dc:creator>
  <dc:creator>Gafurov, Abror</dc:creator>
  <dc:creator>Duethmann, Doris</dc:creator>
  <dc:creator>Barandun, Martina</dc:creator>
  <dc:creator>Merza, Bruno</dc:creator>
  <dc:date>2019-04-01</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Water stable isotope signatures can provide valuable insights into the catchment  internal runoff processes. However, the ability of the water isotope data to constrain  the internal apportionments of runoff components in hydrological models for  glacierized basins is not well understood. This study developed an approach to  simultaneously model the water stable isotopic compositions and runoff processes in  a glacierized basin in Central Asia. The fractionation and mixing processes of water  stable isotopes in and from the various water sources were integrated into a glacio- hydrological model. The model parameters were calibrated on discharge, snow cover  and glacier mass balance data, and additionally isotopic composition of streamflow.  We investigated the value of water isotopic compositions for the calibration of model  parameters, in comparison to calibration methods without using such measurements.  Results indicate that: (1) The proposed isotope-hydrological integrated modeling  approach was able to reproduce the isotopic composition of streamflow, and improved  the model performance in the evaluation period; (2) Involving water isotopic  composition for model calibration reduced the model parameter uncertainty, and  helped to reduce the uncertainty in the quantification of runoff components; (3) The  isotope-hydrological integrated modeling approach quantified the contributions of  runoff components comparably to a three-component tracer-based end-member  mixing analysis method for summer peak flows, and required less water tracer data.  Our findings demonstrate the value of water isotopic compositions to improve the  quantification of runoff components using hydrological models in glacierized basins.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/307694</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/307694/files/bar_chm.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jhydrol.2019.01.048</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Journal of Hydrology. - 2019, vol. 571, p. 332–348</dc:source>
  <dc:subject>info:eu-repo/classification/udc/556</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Constraining hydrological model parameters using water isotopic compositions in a glacierized basin, Central Asia</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
