首页> 外文期刊>Journal of hydrologic engineering >Streamflow Drought Interpreted Using SWAT Model Simulations of Past and Future Hydrologic Scenarios: Application to Neches and Trinity River Basins, Texas
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Streamflow Drought Interpreted Using SWAT Model Simulations of Past and Future Hydrologic Scenarios: Application to Neches and Trinity River Basins, Texas

机译:使用SWAT模型模拟解释过去和将来的水文情景中的径流干旱:在得克萨斯州内什河和三位一体河流域中的应用

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In water resources and environmental management, hydrologic indexes are often valued as decision support tools because of their practical interpretability. This is true with the streamflow drought index (SDI), which is considered to be a relevant tool for assessing the availability of water resources at the watershed level. Hence, the future of freshwater resources at the watershed scale could be better understood by achieving a realistic projection of SDI. This study used a process-based watershed modeling approach to describe a framework for SDI projection. Specifically, the Soil and Water Assessment Tool (SWAT) model was used to simulate distinctly two watersheds located in the state of Texas, the Trinity and the Neches River Basins. The SWAT model was calibrated with monthly streamflow data for the period 1990-1995. The model was subsequently validated with two decades of discharge data (1996-2015). The evaluation of the SWAT performance during the calibration and validation stages showed acceptable values of efficiency criteria for both watersheds (i.e., Nash-Sutcliffe efficiency ranging from 0.56 to 0.65; index of agreement from 0.79 to 0.92). The calibrated model was used to simulate runoff for the future period 2041-2070 using inputs retrieved from a future climate scenario. However, the SDI calculation requires knowledge of the probability distribution of cumulative discharge data. A Kolmogorov-Smirnov's goodness-of-fit analysis was conducted for both observed and simulated cumulative discharges. A lognormal distribution was considered for estimating time series of SDI. For the period 1996-2015, the SDI values recovered from the SWAT simulations matched closely with those derived directly from the observed discharge data (0.52 = R2 = 0.91 for the Neches River, and 0.79 = R2 = 0.89 for the Trinity River). This result demonstrated the capacity of the analytical procedure to capture and project realistically SDI signals. However, analysis of the chi 2 statistic of the SDI patterns for the past and the future periods did not reveal any significant difference. (c) 2019 American Society of Civil Engineers.
机译:在水资源和环境管理中,水文指数由于具有实用的可解释性,因此经常被视为决策支持工具。径流干旱指数(SDI)确实如此,它被认为是评估流域一级水资源可用性的相关工具。因此,通过实现SDI的实际预测,可以更好地理解流域范围内淡水资源的未来。本研究使用基于过程的分水岭建模方法来描述SDI投影的框架。具体而言,使用土壤和水评估工具(SWAT)模型来分别模拟位于得克萨斯州的三位一体流域和内什河流域。使用1990-1995年期间的每月流量数据对SWAT模型进行了校准。随后,使用二十年的排放数据(1996-2015年)验证了该模型。在校准和验证阶段对SWAT性能的评估显示了两个流域效率标准的可接受值(即Nash-Sutcliffe效率从0.56到0.65;一致性指数从0.79到0.92)。校准的模型用于使用从未来气候情景中获取的输入来模拟未来2041-2070年的径流。但是,SDI计算需要了解累积排放数据的概率分布。对观察到的和模拟的累积排放量进行了Kolmogorov-Smirnov拟合优度分析。考虑对数正态分布以估计SDI的时间序列。在1996年至2015年期间,从SWAT模拟中恢复的SDI值与直接从观测到的排放数据中得出的SDI值非常接近(内切斯河为0.52 <= R2 <= 0.91,三位一体为0.79 <= R2 <= 0.89河)。该结果证明了分析程序能够捕获和实际投射SDI信号的能力。但是,对过去和未来SDI模式的chi 2统计量的分析没有发现任何显着差异。 (c)2019美国土木工程师学会。

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