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The runoff simulation and the effect of human activities on runoff in the Source Area of Three Rivers

机译:三条河流源区径流径流模拟及人类活动的影响

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Applying actual meterage statistical data of precipitation, temperature, evaporation and runoff, Using Excel and SPSS software and multi-linear regression analysis, researched the change of hydrological environment and assessed artificial effects on inartificial runoff in the Source Area of Three Rivers. It is concluded that runoff change takes on leading characteristic and the region is start-up area of runoff change. Temperature and precipitation have the effect to increase runoff, evaporation has the effect to reduce runoff and artificial effect on runoff was lesser before 1982. The artificial effects on runoff had increase trend after 1983. The artificial effects are all under 50 percent in Jimai and Tangnaihai and from 50 percent to 80 percent in Huangheyan in most years. The dominant factors which influenced runoff change are natural factors in the east and artificial factors in the west in the source of Yellow River, namely there is the regional difference of fierceness in the west and feebleness on artificial effects on runoff, the closer to headstream area, the stronger artificial effects are.
机译:使用Excel和SPSS软件和多线性回归分析应用实际测量的降水,温度,蒸发和径流数据,研究了水文环境的变化,并评估了三条河流源区中的人工径流的人工效应。结论是,径流变化采用领先的特征,该地区是径流变化的启动区域。温度和沉淀具有增加径流的效果,蒸发有效果,以减少径流和径流的人工效果在1982年之前较小。1983年后的对径流的人工效应增加了趋势。人工效应在吉马和唐尼海的50%以下在大多数年份,Huangheyan的50%至80%。其影响径流变化的主导因素是在黄河源西向东和人为因素自然因素,即有激烈的西部和软弱上径流人工效应,越接近源头区的区域差异,较强的人工效果是。

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