使用SWAT对小型有测量和无测量的山区流域进行水文建模——以印度西高止山脉为例

K. Narula, S. Nischal
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引用次数: 3

摘要

山区森林流域是重要的水文系统,负责世界许多地区的大部分供水和径流计划。在印度,西高止山脉是位于半岛南部地区的重要水文系统之一。这些流域中有几个是未经测量的。土壤和水评估工具(SWAT)已用于模拟两个山区森林流域的流量,即古鲁普尔(699平方公里)(一个测量流域)和上帕亚斯维尼(44.6平方公里)。使用测量流域的月流量和日流量数据进行模型校准和验证。在有限的时间内获得的样本流量值用于验证未经测量的流量。流量-持续时间曲线(FDCs)已被导出以评估每厘米的流量分布。使用Nash-Sutcliffe系数(ENS)、百分比偏差(PBIAS)、终止系数(R2)以及从观察到的和模拟的FDC获得的百分比流量值的比较来评估模型性能。用Latin Hypercube One-factor-At-Time(LH-OAT)进行的敏感性分析指出了五个与土壤土地利用相关的参数,即土壤有效水容量(SOL_AWC)、土壤蒸发补偿因子(ESCO)、土壤深度(SOL_Z)和层、地下水基流(ALPHA_BF)和曲线数(CN2(森林和农业)),敏感地模拟测量和未测量的潮湿山地森林流域。研究表明,在这种流域中,来自动态亚表层区域的横向流对总产水量有着实质性的贡献。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrological Modelling of Small Gauged and Ungauged Mountainous Watersheds Using SWAT—A Case of Western Ghats in India
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 km2) (a gauged watershed) and Upper Payaswini (44.6 km2) (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 (ENS), percent bias (PBIAS), coefficient of de-termination (R2) 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.
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