Water Practice and Technology (Oct 2021)

Modelling streamflow and sediment yield using Soil and Water Assessment Tool: a case study of Lidder watershed in Kashmir Himalayas, India

  • Sarvat Gull,
  • Shagoofta Rasool Shah

DOI
https://doi.org/10.2166/wpt.2021.082
Journal volume & issue
Vol. 16, no. 4
pp. 1370 – 1385

Abstract

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The conjunction of heavy snowfall during winters and intensive rainfall during monsoons along with the mountainous topography expose the Lidder watershed to serious erosion and flood aggravation issues. Barely any attempts have been made for an in-depth examination of the Lidder watershed for precise estimation of sub-basin level runoff and erosion. In this study, the Soil and Water Assessment Tool (SWAT) was calibrated using the Sequential Uncertainty Fitting algorithm (SUFI-2) for modelling streamflow and sediment yield of the Lidder watershed. Daily runoff and sediment event data from 2003–2013 were used in this study; data from 2003–2008 was used for calibration and 2009–2013 for validation. Model performance was evaluated using various statistical tools, which showed good results revealing excellent potential of the SWAT model to simulate streamflow and sediment yield for both calibration and validation periods. The annual rate of average upland sediment drawn from the watershed was approximately 853.96 Mg/ha for an average surface runoff of 394.15 mm/year. This study identifies the vulnerable areas of the Lidder watershed, which can be thoroughly examined by decision-makers for effective management and planning. Further, the calibrated model can be applied to other watersheds with similar characterization to influence strategies in the management of watershed processes. HIGHLIGHTS Kashmir valley is vulnerable to natural hazards.; Assessment of hydrological processes is a significant test for watershed planning.; SWAT model has proven to be an effective tool for prediction of streamflow and sediment yield of mountainous watersheds with complex topography.; Increased degree of soil erosion in the Lidder watershed may be attributed to steep slopes and atrocious land use of its upland sub-basins.;

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