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Modelling potential impacts of climate change on water and nitrate export from a mid-sized, semiarid watershed in the US Southwest

机译:模拟美国西南部中型半干旱流域的气候变化对水和硝酸盐出口的潜在影响

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摘要

The impacts of climate change on water and nitrogen cycles in arid central Arizona (USA) were investigated by integrating the Second Generation Coupled Global Climate Model (CGCM2) and a widely used, physical process-based model, Soil and Water Assessment Tool (SWAT). With statistically downscaled daily climate data from the CGCM2 as model input, SWAT predicted increased potential evapotranspiration and decreased surface runoff, lateral flow, soil water, and groundwater recharge, which suggests serious consequences for the water cycle in this desert catchment in the future. Specifically, stream discharge is projected to decrease by 31 % in the 2020s, 47 % in the 2050s, and 56 % in the 2080s compared to the mean discharge for the base period (0.73 m(3)/s). A flow-duration analysis reveals that the projected reduction of stream discharge in the future is attributable to significant decreases in mid-range and low-flow conditions; however, flood peaks would show a slight increase in the future. The drier and hotter future also will decrease the rate of nitrogen mineralization in the catchment and ultimately, nitrate export from the stream. Since mean mineralization rate would decrease by 15 % in the 2020s, 28 % in the 2050s, and 35 % in the 2080s compared to the based period (9.3 g N ha(-1) d(-1)), the combined impact of reduced catchment mineralization and reduced streamflow would predict declining nitrate export: from today's mean value of 30 kg N/d, to 20, 15 and 12 kg N/d by the 2020s, 2050s, and 2080s, respectively.
机译:通过整合第二代耦合全球气候模型(CGCM2)和广泛使用的基于物理过程的模型土壤和水评估工具(SWAT),研究了气候变化对亚利桑那州中部干旱地区(美国)的水和氮循环的影响。 。利用来自CGCM2的统计缩减的每日气候数据作为模型输入,SWAT预测了潜在的蒸散量增加以及地表径流,侧向流量,土壤水和地下水补给的减少,这预示着未来该沙漠流域的水循环将遭受严重后果。具体而言,与基准时期的平均流量(0.73 m(3)/ s)相比,预计到2020年代,河流流量减少31%,到2050年代减少47%,到2080年代减少56%。流量持续时间分析表明,预计未来河流流量的减少可归因于中流量和低流量条件的显着减少。但是,未来洪灾高峰将有所增加。较干燥和较热的未来也将降低流域中氮矿化的速率,并最终降低溪流中的硝酸盐出口。由于与基准时期(9.3 g N ha(-1)d(-1)相比,2020年代平均矿化率将下降15%,2050年代下降28%,2080年代下降35%,流域矿化的减少和水流的减少将预示硝酸盐出口量的下降:到2020年代,2050年代和2080年代,从今天的平均值30 kg N / d分别降至20、15和12 kg N / d。

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