• DocumentCode
    1703397
  • Title

    Assessment of hydrological regime alteration in the Naoli River since the 1950s

  • Author

    Liu, Guihua ; Luan, Zhaoqing ; Yan, Baixing

  • Author_Institution
    Key Lab. of Wetland Ecology & Environ., CAS, Changchun, China
  • Volume
    2
  • fYear
    2011
  • Firstpage
    951
  • Lastpage
    955
  • Abstract
    The temporal variability of daily runoff from 1956 to 2005 in Baoqing station, which is located in the upper reaches of Naoli River, had been analyzed in the present study. The Mann-Kendall statistical test was applied to assess the changes of the hydrological features in the station and the jump of trends was 1966. Therefore, the runoff records of Baoqing station was divided into two stages namely the period of more natural or less altered flow conditions (1956-1966) and the period of more altered conditions (1967-2005). Then, the Rang of Variability Approach (RVA) proposed by Richer was used to analyze the hydrological situation changes in the upper watershed of Naoli River. The results showed that the human events have tremendously changed the hydrological regime of the upstream of Naoli River and the ecological environment has been destructed to a certain extent. In the future, the mankind´s activities in the watershed should be decreased opportunely.
  • Keywords
    ecology; hydrological techniques; rivers; statistical analysis; AD 1956 to 2005; AD 1966; Baoqing station; Mann-Kendall statistical test; Naoli River; daily runoff; ecological environment; hydrological features; hydrological regime alteration assessment; hydrological situation changes; rang variability approach; temporal variability; upper watershed; hydrological regime; indicators of hydrologic alteration(IHA); range of variability approach(RVA); the Naoli River Basin;
  • fLanguage
    English
  • Publisher
    ieee
  • Conference_Titel
    Water Resource and Environmental Protection (ISWREP), 2011 International Symposium on
  • Conference_Location
    Xi´an
  • Print_ISBN
    978-1-61284-339-1
  • Type

    conf

  • DOI
    10.1109/ISWREP.2011.5893168
  • Filename
    5893168