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Impacts of Climate Change on Water Resources in the Yellow River Basin

机译:气候变化对黄河流域水资源的影响

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Climate change is one of the main reasons of water resources decrease and ecological deterioration in the Yellow River basin in recent years. The WEP-L distributed hydrological model was applied in this paper to analyze the influence of climate change on water resources during the past fifty years, and analyze the response of water resources to the main climate factors such as precipitation and air temperature in the headwater area of the Yellow River basin and the sub-basin of Yiluo river, a tributary in middle reaches of the Yellow River as studied area. The results demonstrated that under the impacts of climate change, the change of water resource from 1980 to 2000 compared with that from 1956 to 1979 were as follows: surface water resources decreased 3.03 billion m3, groundwater resources decreased 2.50 billion m3 with 380 million m3 decrease of the groundwater non-overlapped with surface water, and the total water resources decreased 3.42 billion m3. With increase of air temperature, the total water resources decreased with the decrease of surface water resources and groundwater, and the groundwater non-overlapped with surface water changed little. The tendency of total water resources and its composition was the same as change of precipitation. The responses of monthly runoff to air temperature varied with seasons. The responses of monthly runoff to precipitation change could be divided into three phases, the dry season phase, the wet season phase, and the transitionary season phase.
机译:气候变化是近年来黄河流域水资源减少和生态恶化的主要原因之一。本文采用WEP-L分布式水文模型,分析了过去50年气候变化对水资源的影响,分析了水资源对主要气候因素的响应,如源头地区的降水和气温。黄河流域和伊洛河次流域(黄河中游支流)为研究区域。结果表明,在气候变化的影响下,1980年至2000年与1956年至1979年相比的水资源变化为:地表水资源减少了30.3亿立方米,地下水减少了20.5亿立方米,减少了3.8亿立方米。的地下水没有与地表水重叠,总水资源减少了34.2亿立方米。随着气温的升高,总水资源量随着地表水资源和地下水的减少而减少,而未与地表水重叠的地下水变化不大。总水资源的趋势及其组成与降水变化相同。每月径流对气温的响应随季节而变化。月径流对降水变化的响应可以分为三个阶段,旱季阶段,雨季阶段和过渡季节阶段。

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