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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

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 Q and 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). (C) 2016 Elsevier B.V. All rights reserved.
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(Rc)对降水的弹性(P) ),潜在的蒸散量(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)的集水特征的影响,而在潮湿地区(E-0 / P <1),对于m>的情况,气候条件起着更重要的作用。 2,而流域特征对m <2的影响更大。15个流域中的14个流域的年Q和Rc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,减少的E-0导致Q和R-c分别增加6.30%和7.73%。土地利用/覆盖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随植被覆盖率显着线性下降(p <0.01)。此外,在所有流域,R-c随测量面积的百分比线性下降(其中8个在统计学上具有显着性,p <0.05)。 (C)2016 Elsevier B.V.保留所有权利。

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