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Attribution analysis of climatic and multiple anthropogenic causes of runoff change in the Loess Plateau-A case-study of the Jing River Basin

机译:黄土高原径流变化气候变化的气候与多次人为原因的归因分析 - 以泾河流域为例

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Over the past five decades, under the joint influence of climate change and human activity, river runoff in most areas of Loess Plateau showed a significant declining trend, which poses a great threat to ecological security and land degradation and soil erosion control. To identify the key factors controlling this decline and quantify the contribution rates of the multiple factors, a runoff simulation was established based on the Soil Water Assessment Tool (SWAT), and the influence of climatic and anthropogenic factors on runoff change was calculated by comparing the results of the simulation based on different modeling scenarios. First, the impact of climatic factors on runoff change was gradually decreasing over time, and the anthropogenic factors' impact was increasing based on the runoff observations. Second, the SWAT model proved to be reliable and acceptable for both the calibration and the validation periods, with R- 2 and Nash-Sutcliffe efficiency values both above .8. Third, the influence of climatic factors decreases from 85.70% to 42.43% but that of anthropogenic factors increases from 14.3% to 57.57% in different subperiods. Among the anthropogenic factors, the influence of the direct factor (water withdrawal) is growing the fastest, and the influence of indirect factors is increasing continuously. Therefore, future ecological management and water-related planning in Loess Plateau should consider the importance of human activity and the relationship between humans and the Earth. Finally, a range of comprehensive countermeasures are proposed to assist with sustainable watershed management in the Loess Plateau.
机译:在过去的五十年中,在气候变化和人类活动的联合影响下,黄土高原大多数地区的河流径流显示出了显着下降的趋势,这对生态安全和土地退化和土壤侵蚀控制构成了很大的威胁。为了确定控制这种下降并量化多因素的贡献率的关键因素,基于土壤水评估工具(SWAT)建立径流模拟,并通过比较来计算气候和人为因素对径流变化的影响基于不同建模方案的仿真结果。首先,气候因素对径流变化的影响随着时间的推移逐渐减少,基于径流观察,人为因素的影响正在增加。其次,SWAT模型证明是校准和验证期间的可靠性和可接受的,R-2和NASH-SUTCLIFFE效率值均高于.8。第三,气候因子的影响从85.70%降至42.43%,但是人为因子的影响从不同亚内联的14.3%增加到57.57%。在人为因素中,直接因素(抽取)的影响最快,间接因子的影响持续增加。因此,黄土高原未来生态管理和水有关规划应考虑人类活动的重要性和人类与地球之间的关系。最后,提出了一系列全面的对策,以协助黄土高原可持续分水岭管理。

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