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首页> 外文期刊>Hydrological Processes >Quantifying the effects of climate variability and human activities on runoff from the Laohahe basin in northern China using three different methods (pages 2492–2505)
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Quantifying the effects of climate variability and human activities on runoff from the Laohahe basin in northern China using three different methods (pages 2492–2505)

机译:使用三种不同方法量化气候变化和人类活动对中国北方老哈河流域径流的影响(第2492–2505页)

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Much attention has recently been focused on the effects that climate variability and human activities have had on runoff.nIn this study, these effects are quantified using three methods, namely, multi-regression, hydrologic sensitivity analysis, andnhydrologic model simulation. A conceptual framework is defined to separate the effects. As an example, the change in annualnrunoff from the semiarid Laohahe basin (18 112 km2) in northern China was investigated. Non-parametric Mann-Kendall test,nPettitt test, and precipitation-runoff double cumulative curve method were adopted to identify the trends and change-pointsnin the annual runoff from 1964 to 2008 by first dividing the long-term runoff series into a natural period (1964–1979) and anhuman-induced period (1980–2008). Then the three quantifying methods were calibrated and calculated, and they providednconsistent estimates of the percentage change in mean annual runoff for the human-induced period. In 1980–2008, humannactivities were the main factors that reduced runoff with contributions of 89–93%, while the reduction percentages duento changes in precipitation and potential evapotranspiration only ranged from 7 to 11%. For the various effects at differentndurations, human activities were the main reasons runoff decreased during the two drier periods of 1980–1989 and 2000–2008.nIncreased runoff during the wetter period of 1990–1999 is mainly attributed to climate variability. This study quantitativelynseparates the effects of climate variability and human activities on runoff, which can serve as a reference for regional waternresources assessment and management. Copyright  2011 John Wiley & Sons, Ltd.
机译:最近,人们已经将许多注意力集中在气候变化和人类活动对径流的影响上。n在这项研究中,使用多重回归,水文敏感性分析和水文模型模拟这三种方法来量化这些影响。定义了一个概念框架来分离效果。例如,研究了中国北方半干旱老哈河盆地(18 112 km2)年径流量的变化。首先通过将长期径流序列划分为自然周期,采用非参数Mann-Kendall检验,nPettitt检验和降水径流双累积曲线方法来确定1964年至2008年年径流量的趋势和变化点。 1964–1979年)和非人为诱导的时期(1980–2008年)。然后对这三种定量方法进行了校准和计算,它们提供了关于人为期平均年径流量百分比变化的一致估计。在1980年至2008年期间,人类活动是减少径流的主要因素,其贡献为89%至93%,而由于降水变化和潜在的蒸散作用而导致的减少百分比仅为7%至11%。由于不同的影响,人类活动是径流在1980-1989和2000-2008的两个干旱时期减少的主要原因。n在1990-1999较湿的时期径流增加主要归因于气候多变性。本研究定量分析了气候变化和人类活动对径流的影响,可为区域水资源评估和管理提供参考。版权所有©2011 John Wiley&Sons,Ltd.

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