<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>Wei, Ren-juan</dc:creator>
  <dc:creator>Peng, Liang</dc:creator>
  <dc:creator>Liang, Chuan</dc:creator>
  <dc:creator>Haemmig, Christoph</dc:creator>
  <dc:creator>Huss, Matthias</dc:creator>
  <dc:creator>Mu, Zhen-xia</dc:creator>
  <dc:creator>He, Ying</dc:creator>
  <dc:date>2019-03-01</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Yarkant River is a tributary of Tarim River in China, and the basin lacks observational  data. To investigate past climatic variations and predict future climate changes,  precipitation, air temperature and runoff data from Kaqun hydrological station are  analysed at monthly and seasonal scales using detrended fluctuation analysis (DFA).  Results show that DFA scaling exponents of monthly precipitation, air temperature  and runoff are 0.535, 0.662 and 0.582, respectively. These three factors all show long- range correlations. Their increasing trends will continue in the near future as the  climate shifts towards warmer and more humid. Spring and winter precipitation exhibit  long-range correlations and will increase in the future. In contrast, summer and  autumn precipitation exhibits random fluctuations and does not show stable trends. Air  temperature during all seasons exhibits long-range correlations and will continue to  increase in the future. Runoff during the spring and summer exhibits weak anti- persistence, but autumn and winter runoff show long-range correlations and  increasing trends. The vertical distribution of precipitation was first analysed using  observed data and climate reanalysis data. It indicates that precipitation increases  with elevations below 2,000 m a.s.l. at a rate of 26 mm per 100 m and decreases with  elevations above 2,000 m a.s.l.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/307735</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/307735/files/hus_ats.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.2166/wcc.2018.111</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Journal of Water and Climate Change. - 2019, vol. 10, no. 1, p. 167–180</dc:source>
  <dc:subject>info:eu-repo/classification/udc/556</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Analysis of temporal and spatial variations in hydrometeorological elements in the Yarkant River Basin, China</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
