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Impacts of climate change on stream flow and water quality in a drinking water source area, Northern China

机译:气候变化对中国北方饮用水源地区河流流量和水质的影响

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Understanding the impacts of climate change on water quality and stream flow is important for management of water resources and environment. Miyun Reservoir is the only surface drinking water source in Beijing, which is currently experiencing a serious water shortage. Therefore, it is vital to identify the impacts of climate change on water quality and quantity of the Miyun Reservoir watershed. Based on long-time-series data of meteorological observation, future climate change scenarios for this study area were predicted using global climate models (GCMs), the statistical downscaling model (SDSM), and the National Climate Centre/Gothenburg University-Weather Generator (NWG). Future trends of nonpoint source pollution load were estimated and the response of nonpoint pollution to climate change was determined using the Soil and Water Assessment Tool (SWAT) model. Results showed that the simulation results of SWAT model were reasonable in this study area. The comparative analysis of precipitation and air temperature simulated using the SDSM and NWG separately showed that both tools have similar results, but the former had a larger variability of simulation results than the latter. With respect to simulation variance, the NWG has certain advantages in the numerical simulation of precipitation, but the SDSM is superior in simulating precipitation and air temperature changes. The changes in future precipitation and air temperature under different climate scenarios occur basically in the same way, that is, an overall increase is estimated. Particularly, future precipitation will increase significantly as predicted. Due to the influence of climate change, discharge, total nitrogen (TN) and total phosphorus (TP) loads from the study area will increase over the next 30 years by model evaluation. Compared to average value of 1961 similar to 1990, discharge will experience the highest increase (15%), whereas TN and TP loads will experience a smaller increase with a greater range of annual fluctuations of 2021 similar to 2050.
机译:了解气候变化对水质和水流的影响对水资源和环境的管理很重要。密云水库是北京唯一的地表饮用水水源,目前正面临严重的水资源短缺。因此,确定气候变化对密云水库流域水质和水量的影响至关重要。根据气象观测的长期序列数据,使用全球气候模型(GCM),统计缩减模型(SDSM)和国家气候中心/哥德堡大学天气生成器( NWG)。估算了面源污染负荷的未来趋势,并使用土壤和水评估工具(SWAT)模型确定了面源污染对气候变化的响应。结果表明,SWAT模型的仿真结果在该研究区域是合理的。使用SDSM和NWG分别模拟的降水和气温的对比分析表明,两种工具的结果相似,但前者的模拟结果比后者更大。关于模拟方差,NWG在降水的数值模拟中具有某些优势,但SDSM在模拟降水和气温变化方面具有优势。在不同气候情景下,未来降水和气温的变化基本上以相同的方式发生,即估计总体增加。特别是,未来的降水将如预期的那样显着增加。由于气候变化的影响,通过模型评估,研究区域的排放,总氮(TN)和总磷(TP)负荷将在未来30年内增加。与1961年(与1990年相似)的平均值相比,排放量将经历最高的增长(15%),而TN和TP负荷将经历较小的增长,与2050年相似的2021年年度波动范围更大。

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