4.6 Article

Application of SWAT in Hydrological Simulation of Complex Mountainous River Basin (Part I: Model Development)

Journal

WATER
Volume 13, Issue 11, Pages -

Publisher

MDPI
DOI: 10.3390/w13111546

Keywords

hydrological simulation; SWAT; water balance; complex mountain; Budhigandaki

Funding

  1. University Grants Commission (UGC), Nepal

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The study used the SWAT hydrological model to characterize the rainfall-runoff behavior in the Budhigandaki River Basin in central Nepal, and assessed the model's applicability in a complex mountainous river basin. The model performance was ranked as very good, with the study providing additional evidence of SWAT's ability to simulate rainfall-runoff characteristics in such complex catchments.
The soil and water assessment tool (SWAT) hydrological model has been used extensively by the scientific community to simulate varying hydro-climatic conditions and geo-physical environment. This study used SWAT to characterize the rainfall-runoff behaviour of a complex mountainous basin, the Budhigandaki River Basin (BRB), in central Nepal. The specific objectives of this research were to: (i) assess the applicability of SWAT model in data scarce and complex mountainous river basin using well-established performance indicators; and (ii) generate spatially distributed flows and evaluate the water balance at the sub-basin level. The BRB was discretised into 16 sub-basins and 344 hydrological response units (HRUs) and calibration and validation was carried out at Arughat using daily flow data of 20 years and 10 years, respectively. Moreover, this study carried out additional validation at three supplementary points at which the study team collected primary river flow data. Four statistical indicators: Nash-Sutcliffe efficiency (NSE), percent bias (PBIAS), ratio of the root mean square error to the standard deviation of measured data (RSR) and Kling Gupta efficiency (KGE) have been used for the model evaluation. Calibration and validation results rank the model performance as very good. This study estimated the mean annual flow at BRB outlet to be 240 m(3)/s and annual precipitation 1528 mm with distinct seasonal variability. Snowmelt contributes 20% of the total flow at the basin outlet during the pre-monsoon and 8% in the post monsoon period. The 90%, 40% and 10% exceedance flows were calculated to be 39, 126 and 453 m(3)/s respectively. This study provides additional evidence to the SWAT diaspora of its applicability to simulate the rainfall-runoff characteristics of such a complex mountainous catchment. The findings will be useful for hydrologists and planners in general to utilize the available water rationally in the times to come and particularly, to harness the hydroelectric potential of the basin.

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