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首页> 外文期刊>The Science of the Total Environment >Determining the hydrological responses to climate variability and land use/cover change in the Loess Plateau with the Budyko framework
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Determining the hydrological responses to climate variability and land use/cover change in the Loess Plateau with the Budyko framework

机译:利用Budyko框架确定黄土高原地区对气候变化和土地利用/覆盖变化的水文响应

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摘要

Understanding and quantifying the impacts of land use/cover change and climate variability on hydrological responses are important to the design of water resources and land use management strategies for adaptation to climate change, especially in water-limited areas. The elasticity method was used to detect the responses of streamflow and runoff coefficient to various driving factors in 15 main catchments of the Loess Plateau, China between 1961 and 2009. The elasticity of streamflow (Q) and runoff coefficient (R_c) to precipitation (P), potential evapotranspiration (E_0), and catchment characteristics (represented by the parameter m in Fu's equation) were derived based on the Budyko hypothesis. There were two critical values of m = 2 and E_0/P = 1 for the elasticity of Qand R_c. The hydrological responses were mainly affected by catchment characteristics in water-limited regions (E_0/P > 1), and in humid areas (E_0/P < 1), climate conditions played a more important role for cases of m > 2 whereas catchment characteristics had a greater impact for cases of m < 2. The annual Q and R_c in 14 of the 15 catchments significantly decreased with average reduction of 0.87 mm yr~(-1) and 0.18% yr~(-1), respectively. The mean elasticities of Q to P, E_0 and m were 2.66, - 1.66 and - 3.17, respectively. The contributions of land use/ cover change and P reduction to decreased Q were 64.75% and 41.55%, respectively, while those to decreased R_c were 75.68% and 32.06%, respectively. In contrast, the decreased E_0 resulted in 6.30% and 7.73% increase of Q and R_c, respectively. The contribution of land use/cover changes was significantly and positively correlated with the increase in the percentage of the soil and water conservation measures area (p < 0.05). The R_c significantly and linearly decreased with the vegetation coverage (p < 0.01). Moreover, the R_c linearly decreased with the percentage of measures area in all catchments (eight of them were statistically significant with p < 0.05).
机译:理解和量化土地利用/覆盖变化和气候变化对水文响应的影响,对于设计水资源和土地利用管理战略以适应气候变化(特别是在水禁区)至关重要。利用弹性方法检测了1961-2009年黄土高原15个主要流域径流和径流系数对各种驱动因子的响应。径流(Q)和径流系数(R_c)对降水的弹性(P ),潜在蒸散量(E_0)和集水特征(由Fu方程中的参数m表示)是根据Budyko假设得出的。对于Q和R_c的弹性,有两个临界值m = 2和E_0 / P = 1。水文响应主要受缺水地区(E_0 / P> 1)和集水区特征(E_0 / P <1)的集水特征影响,在m> 2的情况下,气候条件起着更重要的作用,而集水特征对m <2的影响更大。15个流域中有14个流域的年Q和R_c显着下降,分别平均降低0.87 mm yr〜(-1)和0.18%yr〜(-1)。 Q对P,E_0和m的平均弹性分别为2.66,-1.66和-3.17。土地利用/覆被变化和磷减少对降低Q的贡献分别为64.75%和41.55%,而对R_c降低的贡献分别为75.68%和32.06%。相反,降低的E_0导致Q和R_c分别增加6.30%和7.73%。土地利用/覆被变化的贡献与水土保持措施面积百分比的增加显着正相关(p <0.05)。 R_c随植被覆盖度显着线性下降(p <0.01)。此外,在所有流域,R_c随测量面积的百分比呈线性下降(其中8个在统计学上具有显着性,p <0.05)。

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  • 来源
    《The Science of the Total Environment》 |2016年第1期|331-342|共12页
  • 作者单位

    State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China,Joint Center for Global Change Studies, Beijing 100875, China;

    State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China,Joint Center for Global Change Studies, Beijing 100875, China;

    State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China,Joint Center for Global Change Studies, Beijing 100875, China;

    College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062, China;

    College of Urban and Environmental Sciences, Northwest University, Xi'an 710027, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Streamflow; Runoff coefficient; Climate variability; Land use/cover change; Elasticity method; Loess Plateau;

    机译:水流;径流系数;气候多变性;土地利用/覆盖变化;弹性法;黄土高原;

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