Ground water availability assessment for a data-scarce river basin in Nepal using SWAT hydrological model

Water Supply Pub Date : 2023-12-20 DOI:10.2166/ws.2023.332
Raghu Nath Prajapati, Nurazim Ibrahim, Manish Kumar Goyal, Bhesh Raj Thapa, Koshish Raj Maharjan
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Abstract

Mountainous river basins are expected to experience significant seasonal fluctuations in water supply due to climate change. Thus, hydrological modeling becomes further challenging while accounting for data-scarce mountainous basins observing climate change impacts. In this study, Soil and Water Assessment Tool (SWAT) was used to predict hydrological flow in the Sunkoshi River Basin (SRB) based on daily rainfall and temperature data spanning 36 years. The specific objectives of this study were as follows: (i) to use the SWAT model to simulate the long-term hydrological response, (ii) to generate spatially distributed rainfall–runoff and subbasin-wise water balance components using well-established performance indicators. Calibration and validation at the outlet of the study area were successful, with the values of R2/Nash–Sutcliffe efficiency (NSE) calculated as 0.91/0.82 for monthly data and 0.79/0.73 for daily data. In the validation phase, the values of R2/NSE were 0.91/0.84 for monthly data and 0.82/0.75 for daily data, respectively. This study predicted the average yearly flow and precipitation at the SRB outlet to be 279 m3/s and 368.25 mm, respectively. Approximately, 30% of water loss was attributed to evapotranspiration, 18% to runoff, and 30% to lateral flow. The findings of this study will contribute to water resource management.
利用 SWAT 水文模型对尼泊尔数据稀缺的河流流域进行地下水可用性评估
由于气候变化,山区河流流域的供水量预计将出现明显的季节性波动。因此,在考虑到数据稀缺的山区盆地观测气候变化影响的同时,水文建模变得更具挑战性。本研究使用水土评估工具 (SWAT) 根据 36 年的日降雨量和温度数据预测孙越河流域 (SRB) 的水文流量。本研究的具体目标如下(i) 使用 SWAT 模型模拟长期水文响应,(ii) 利用成熟的性能指标生成空间分布的降雨-径流和子流域水量平衡成分。在研究区域出口处的校准和验证都很成功,月数据的 R2/Nash-Sutcliffe 效率(NSE)计算值为 0.91/0.82,日数据的 R2/Nash-Sutcliffe 效率(NSE)计算值为 0.79/0.73。在验证阶段,月数据的 R2/NSE 值分别为 0.91/0.84,日数据的 R2/NSE 值分别为 0.82/0.75。这项研究预测了 SRB 出口的年平均流量和降水量,分别为 279 立方米/秒和 368.25 毫米。约 30% 的水量损失归因于蒸发,18% 归因于径流,30% 归因于侧流。这项研究的结果将有助于水资源管理。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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