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Spatio-temporal patterns of the effects of precipitation variability and land use/cover changes on long-term changes in sediment yield in the Loess Plateau, China

机译:黄土高原地区降水变化和土地利用/覆盖变化对沉积物长期变化影响的时空格局

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pstrongAbstract./strong Within China's Loess Plateau there have been concerted revegetation efforts and engineering measures since the 1950s aimed at reducing soil erosion and land degradation. As a result, annual streamflow, sediment yield, and sediment concentration have all decreased considerably. Human-induced land use/cover change (LUCC) was the dominant factor, contributing over 70span class="thinspace"/span% of the sediment load reduction, whereas the contribution of precipitation was less than 30span class="thinspace"/span%. In this study, we use 50-year time series data (1961a??2011), showing decreasing trends in the annual sediment loads of 15 catchments, to generate spatio-temporal patterns in the effects of LUCC and precipitation variability on sediment yield. The spacea??time variability of sediment yield was expressed notionally as a product of two factors representing (i)??the effect of precipitation and (ii)??the fraction of treated land surface area. Under minimal LUCC, the square root of annual sediment yield varied linearly with precipitation, with the precipitationa??sediment load relationship showing coherent spatial patterns amongst the catchments. As the LUCC increased and took effect, the changes in sediment yield pattern depended more on engineering measures and vegetation restoration campaign, and the within-year rainfall patterns (especially storm events) also played an important role. The effect of LUCC is expressed in terms of a sediment coefficient, i.e., the ratio of annual sediment yield to annual precipitation. Sediment coefficients showed a steady decrease over the study period, following a linear decreasing function of the fraction of treated land surface area. In this way, the study has brought out the separate roles of precipitation variability and LUCC in controlling spatio-temporal patterns of sediment yield at catchment scale./p.
机译:> >摘要。自1950年代以来,在中国的黄土高原地区一直采取协调一致的植被恢复措施和工程措施,旨在减少水土流失和土地退化。结果,年流量,泥沙产量和泥沙浓度都大大降低了。人为导致的土地利用/覆盖变化(LUCC)是主要因素,占沉积物减量的70%以上,而降水量的贡献少于30% =“ thinspace”> %。在这项研究中,我们使用了50年的时间序列数据(1961a-2011年),显示了15个流域的年沉积量减少趋势,从而产生了LUCC和降水变化对沉积物产量的影响的时空格局。沉积物产量的时空变异性在理论上表示为两个因素的乘积,这些因素代表(i)β降水的影响和(ii)β处理土地表面积的分数。在最小LUCC条件下,年产沙量的平方根随降水量线性变化,降水量与泥沙负荷的关系在各流域之间表现出连贯的空间格局。随着LUCC的增加和生效,沉积物产量模式的变化更多地取决于工程措施和植被恢复运动,并且年内降雨模式(尤其是暴风雨事件)也发挥了重要作用。 LUCC的影响以沉积系数表示,即年沉积物产量与年降水量之比。沉积系数在研究期内呈稳定下降趋势,这是处理土地表面积分数线性下降的函数。这样,该研究就揭示了降水变化和LUCC在控制流域尺度上沉积物产量的时空格局中的独立作用。

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