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Contributions of Climate Change and Human Activities to the Runoff Change in Heihe River Valley

机译:黑河流域气候变化和人类活动对径流变化的贡献

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Based on the data of meteorological and hydrological material from 1960 to 2008,this paper used the methods of accumulative anomaly,annual accumulation and rate of change about cumulate slope,and also adopted nonparametric Man-Kendall test.The paper analyzed characteristics and trend of runoff and climate,and calculated the rate of contribution that climate change and human activities caused runoff variation in the upper and middle reaches of Heihe River valley.The results are shown as follows: according to the methods of accumulative anomaly analysis,two inflection points,1979 and 1984,for the accumulative runoff in the upper and middle reaches of Heihe River Basin,were identified respectively.The time series was divided into upstream (1960-1979,1980-2008) and middle (1960-1984,1985-2008) as year of runoff sudden variation,and got linear equation of accumulated runoff,cumulative precipitation and accumulative evapotranspiration with year separately.The upstream climate change was key factors,human activity had less impact.Their contribution rate that increases runoff was 59.71% and 40.29%.Climate varying in the middle influence was little,human activity was main points.The rates that decreased runoff were 25.23% and 74.77% respectively.This research played a role with regards to the water resources in Heihe River Basin development and futureutilization.
机译:基于1960 — 2008年的气象水文资料,采用累积反常,年累积和累积坡度变化率的方法,并采用非参数Man-Kendall检验。分析了径流的特征和趋势。计算得出气候变化和人类活动对黑河流域中上游径流变化的贡献率。结果如下:根据累积异常分析方法,两个拐点,1979年和1984年,分别确定了黑河流域上游和中游的累积径流。时间序列分为上游(1960-1979,1980-2008)和中部(1960-1984,1985-2008)。年径流突变,并分别得到年径流累积量,累积降水量和蒸散量的线性方程。上游气候变化是关键径流增加的贡献率分别为59.71%和40.29%。气候变化的中间影响较小,人为活动是重点。径流减少的贡献率分别为25.23%和74.77%。研究对黑河流域水资源的开发和未来利用发挥了作用。

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