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Regional effects of vegetation restoration on water yield across the Loess Plateau, China

机译:黄土高原地区植被恢复对水产量的区域影响

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The general relationships between vegetation and water yield under different climatic regimes are well established at a small watershed scale in the past century. However, applications of these basic theories to evaluate the regional effects of land cover change on water resources remain challenging due to the complex interactions of vegetation and climatic variability and hydrologic processes at the large scale. The objective of this study was to explore ways to examine the spatial and temporal effects of a large ecological restoration project on water yield across the Loess Plateau region in northern China.We estimated annual water yield as the difference between precipitation input and modelled actual evapotranspiration (ET) output. We constructed a monthly ET model using published ET data derived from eddy flux measurements and watershed streamflow data. We validated the ET models at a watershed and regional levels. The model was then applied to examine regional water yield under land cover change and climatic variability during the implementation of the Grain-for-Green (GFG) project during 1999-2007. We found that water yield in 38% of the Loess Plateau area might have decreased (1-48mm per year) as a result of land cover change alone. However, combined with climatic variability, 37% of the study area might have seen a decrease in water yield with a range of 1-54mm per year, and 35% of the study area might have seen an increase with a range of 1-10mm per year. Across the study region, climate variability masked or strengthened the water yield response to vegetation restoration. The absolute annual water yield change due to vegetation restoration varied with precipitation regimes with the highest in wet years, but the relative water yield changes were most pronounced in dry years. We concluded that the effects of land cover change associated with ecological restoration varied greatly over time and space and were strongly influenced by climatic variability in the arid region. The current regional vegetation restoration projects have variable effects on local water resources across the region. Land management planning must consider the influences of spatial climate variability and long-term climate change on water yield to be more effective for achieving environmental sustainability.
机译:在过去一个世纪的小流域范围内,在不同气候条件下植被与水分产量之间的一般关系已经建立。然而,由于植被与气候变化的复杂相互作用以及大规模的水文过程,将这些基本理论用于评估土地覆盖变化对水资源的区域影响仍然具有挑战性。这项研究的目的是探索检验大型生态修复项目对中国北方黄土高原地区水产量的时空影响的方法。我们将年水产量估算为降水输入与模拟实际蒸散量之间的差异( ET)输出。我们使用从涡流测量和分水岭流量数据得出的已发布ET数据构建了每月ET模型。我们在分水岭和区域级别验证了ET模型。然后,在1999-2007年实施“绿色换粮”(GFG)项目的过程中,该模型用于检验土地覆盖变化和气候变化下的区域水产量。我们发现,仅因土地覆被变化,黄土高原地区38%的水产量可能会下降(每年1-48毫米)。但是,结合气候变化,研究区域的37%的水产量可能会下降,每年范围为1-54mm,而研究区域的35%的水产量可能会以1-10mm的范围增长。每年。在整个研究区域,气候变化掩盖或增强了对植被恢复的水分响应。植被恢复导致的绝对年产量变化随降水变化而变化,在湿润年份最高,而在干旱年份相对产量变化最为明显。我们得出的结论是,与生态恢复相关的土地覆盖变化的影响随时间和空间变化很大,并且受到干旱地区气候变化的强烈影响。当前的区域植被恢复项目对整个区域的当地水资源有不同的影响。土地管理规划必须考虑空间气候变异性和长期气候变化对水产量的影响,以便更有效地实现环境的可持续性。

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