首页> 外文期刊>Journal of Water Resource and Protection >Hydrological Modelling of Small Gauged and Ungauged Mountainous Watersheds Using SWAT—A Case of Western Ghats in India
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Hydrological Modelling of Small Gauged and Ungauged Mountainous Watersheds Using SWAT—A Case of Western Ghats in India

机译:使用SWAT的小衡量和未凝固的山地流域水文建模 - 以印度西船为例

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Mountainous forested watersheds are important hydrologic systems that are responsible for much of the water supply and run-of-the-river hy-dropower schemes in many parts of the world. In India, the Western Ghats are one of such important hydrologic systems located in southern peninsular region. Several of these watersheds are ungauged. The Soil and Water Assessment Tool (SWAT) has been used to model streamflows for two mountainous forested watersheds, namely, Gurupur (699 km~(2)) (a gauged watershed) and Upper Payaswini (44.6 km~(2)) (an ungauged wa-tershed). Model calibration and validation are performed using monthly and daily streamflow data for the gauged watershed. Sample flow values obtained over a limited period were used for validation of ungauged wa-tershed. Flow duration curves (FDCs) have been derived to assess per-centile flow distributions. Model performance is evaluated using Nash-Sutcliffe coefficient ( E _( NS )), percent bias ( PBIAS ), coefficient of de-termination (R~(2)) and comparison of percentile flow values obtained from observed and simulated FDCs. Sensitivity analysis with Latin Hypercube One-factor-At-a-Time ( LH-OAT ) indicates five soil-land use related pa-rameters namely, soil available water capacity (SOL_AWC), soil evapora-tion compensation factor ( ESCO ), soil depth ( SOL_Z ) and layers, groundwater baseflow ( ALPHA_BF ), and curve number ( CN2 (forest & agriculture)), to be sensitive for simulating both gauged and ungauged wet mountainous forested watersheds. Study shows that lateral flows from dynamic sub-surface zones in such watersheds contribute substan-tially to the total water yield.
机译:山区森林的流域是世界许多地方的大部分供水和河流的水资源和河流的大部分水能系统的重要水文系统。在印度,西船是位于南半岛地区的重要水文系统之一。这些流域中的几个都是没有乞讨的。土壤和水评估工具(SWAT)已被用于模拟两个山地森林流域的流动流,即Gurupur(699公里〜(2))(一只测量的水域)和上部Payaswini(44.6公里〜(2))(AN没有戈格氏腰部的沃思曲线)。模型校准和验证使用每月和每日流式流数据进行测量的流域。在有限的时期获得的样品流量值用于验证未凝固的WA-TERSHED。流动持续时间曲线(FDC)已被推导为评估每居住流量分布。使用NASH-SUTCLIFFE系数(E _(NS)),偏差百分比(PBIAS),去终止系数(R〜(2))和从观察到的FDC获得的百分比流量值进行评估模型性能。敏感性分析与拉丁型超立体一体因素 - a-a-time(lh-OAT)表示五个土地利用相关的PA-rameters即土壤可用水容量(Sol_AWC),土壤蒸发补偿因子(ESCO),土壤深度(SOL_Z)和层,地下水基础流(alpha_bf)和曲线数(CN2(森林和amp;农业)),对模拟测量和未凝固的湿山地森林流域进行敏感。研究表明,这种流域中的动态亚表面区的横向流量有助于总水产量。

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