loading page

Streamflow and its components in Ebinur basin: decoupling of anthropogenic and climatic elements
  • +2
  • bao qingling,
  • Ding Jianli,
  • Liu Jie,
  • Han Lijie,
  • Wang Yinghui
bao qingling

Corresponding Author:[email protected]

Author Profile
Ding Jianli
Xinjiang University
Author Profile
Liu Jie
Xinjiang University
Author Profile
Han Lijie
Xinjiang University
Author Profile
Wang Yinghui
Xinjiang University
Author Profile

Abstract

Detecting and assessing changes in the hydrological cycle and how it responds to a changing environment is essential for maintaining regional ecological security and restoring damaged ecosystems. The Ebinur Lake basin, an important ecological barrier in the Junggar Basin of Xinjiang, China, has undergone significant changes in recent decades as a result of massive eco-rehabilitation projects and increased anthropogenic factors. To solve the above defects, we separated the study period into three phases based on the heuristic segmentation algorithm:the reference phase (1964-1985) and two impact phases: I (1986-2000) and II (2001-2017). The Variable Infiltration Capacity (VIC) surface models were used to determine the contribution of both human activities and climate change to streamflow along with its components. Based on the VIC model of streamflow splitting, the results showed that surface runoff, baseflow and snowmelt accounted for 20.97%, 60.37% and 23.42% of the annual runoff volume respectively. The differential evolution Markov chain (DEMC) algorithm improved the Nash-Sutcliffe efficiency by 20% over the traditional SCE-UA algorithm, which exceeded 0.6 and reached reliable level. Increases in cropland and forested land were partially contributed by grassland and heathland throughout the study period, While the leaf area index (LAI) of the season of plant growth showed a trend of 0.002 increase per year. Direct human activity was the main factor in the reduction of runoff in impact phase I and indirect human activity in impact phase II, Whereas, in the total impact phase, climate c