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Using Geospatial Analysis and Hydrologic Modeling to Estimate Climate Change Impacts on Nitrogen Export: Case Study for a Forest and Pasture Dominated Watershed in North Carolina

机译:利用地理空间分析和水文模型来估算气候变化对氮原氮的影响:北卡罗来纳州森林和牧场占地面理的案例研究

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摘要

Many watersheds are currently experiencing streamflow and water quality related problems that are caused by excess nitrogen. Given that weather is a major driver of nitrogen transport through watersheds, the objective of this study was to predict climate change impacts on streamflow and nitrogen export. A forest and pasture dominated watershed in North Carolina Piedmont region was used as the study area. A physically-based Soil and Water Assessment Tool (SWAT) model parameterized using geospatial data layers and spatially downscaled temperature and precipitation estimates from eight different General Circulation Models (GCMs) were used for this study. While temperature change predictions are fairly consistent across the GCMs for the study watershed, there is significant variability in precipitation change predictions across the GCMs, and this leads to uncertainty in the future conditions within the watershed. However, when the downscaled GCM projections were taken as a model ensemble, the results suggest that both high and low emission scenarios would result in an average increase in streamflow of 14.1% and 12.5%, respectively, and a decrease in the inorganic nitrogen export by 12.1% and 8.5%, respectively, by the end of the century. The results also show clear seasonal patterns with streamflow and nitrogen loading both increasing in fall and winter months by 97.8% and 50.8%, respectively, and decreasing by 20.2% and 35.5%, respectively, in spring and summer months by the end of the century.
机译:许多流域目前正在经历由过量的氮气引起的流流和水质相关问题。鉴于天气是通过流域的氮气运输的主要驱动因素,本研究的目的是预测气候变化对流流和氮原氮的影响。在北卡罗来纳皮蒙特地区北卡罗来纳州北卡罗来纳州的森林和牧场被用作研究区。使用地理空间数据层和空间较低的温度和降水估计的物理基地和水评估工具(SWAT)模型来自来自八种不同的一般循环模型(GCMS)的研究。虽然温度变化预测在研究流域的GCMS上相当一致,但在GCMS上的降水变化预测有显着的变化,这导致了流域内未来条件下的不确定性。然而,当较低的GCM投影被作为模型集合时,结果表明,高和低发射场景都会导致流流量分别为14.1%和12.5%的平均增加,并减少无机氮源到本世纪末,分别为12.1%和8.5%。结果还显示出清晰的季节性模式,秋季和冬季月份的流出和氮气加载分别增加了97.8%和50.8%,分别在本世纪末的春季和夏季分别降低了20.2%和35.5% 。

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