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Research on Influences of Global Climate Change on Water Resources in the Yellow River Basin

机译:全球气候变化对黄河流域水资源影响的研究

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The study explored global climate change influence on water resources in Yellow River basin. A HBV hydrological model was developed to simulate the rainfall-runoff relationship at the region. Importing the CCLM climate model data, runoff at Lijin station was obtained in 2000-2039. The results indicate: (1) the annual average runoff depth is 1213mm, runoff in summer is larger than in spring, autumn and winter. The water resources decrease in three months (March, April and Jun) and increase in other months. (2) for inter-annual variations, the water resources increases slightly, and increase trend is about 64.8mm/10a. Water resources are insufficient in 200-2016, and rise gradually from 2017. (3) for different decades, the water resources are lack relatively in 2001-2010 and 2011-2020, and the differences are -59.4mm and -76.0mm respectively. While, the water resources in 2021-2030 and 2031-2039 are abundant, and the differences are 90.6mm and 88.8mm respectively.
机译:该研究探索了黄河流域水资源的全球气候变化影响。开发了HBV水文模型,以模拟该地区的降雨径流关系。进口CCLM气候模型数据,在2000 - 2013年获得了荔枝站的径流。结果表明:(1)年平均径流深度为1213mm,夏季径流大于春季,秋季和冬季。水资源在三个月(4月,4月和君)减少,并在其他几个月增加。 (2)对于年间变异,水资源略有增加,增加趋势约为64.8mm / 10a。水资源在200-2016中不足,从2017年逐渐上升。(3)在不同的数十年中,2001 - 2010年和2011-2020缺乏水资源,分别为-59.4mm和-76.0毫米。虽然,2021-2030和2031-2039的水资源丰富,差异分别为90.6mm和88.8毫米。

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