Analysing hydrological balance of Pindar-Nandakini River Basin, Kumaon Himalaya using SWAT model
DOI:
https://doi.org/10.54386/jam.v27i3.2964Keywords:
SWAT modelling, Glacier valleys, Pindar-Nandakini River Basin, Groundwater recharge, Central HimalayaAbstract
Water availability from the central Himalayan River Basins is threatened by warming-mediated glacier melt and declining precipitation. This study employed the Soil and Water Assessment Tool (SWAT) model to analyze the water balance of the Pindar-Nandakini River Basin (PRB). The model was calibrated and validated using high-resolution data, achieving strong performance (R²: 0.85, NSE: 0.71). Runoff and evapotranspiration (ET) account for approximately 29.7% and 28.9% respectively. Lateral soil flow is a major contributor (23.7% of precipitation), significantly influencing streamflow and groundwater levels. Snowmelt contributes around 10.3%, while deep groundwater flow is minimal. The model considerably simulated seasonal runoff patterns, particularly peak flows during the monsoon. Sediment loading, at 563.1 t ha-1 annually, is a significant concern. The study also underscores the critical role of ET and runoff in the hydrological processes of the basins, revealing potential challenges during high-flow events and climate-driven forest greening trends. These findings emphasize the importance of the SWAT model in understanding the complex hydrological processes within the Himalayan glacier basins, highlighting the basin's vulnerability to climate change impacts, particularly glacier retreat.
References
Arnold, J.G., Moriasi, D.N., Gassman, P.W., Abbaspour, K.C., White, M.J., Srinivasan, R. and Kannan, N., (2013). SWAT: model use, calibration, and validation. Trans. ASABE 55 (4): 1491–1508.
Arnold, J.G., Youssef, M.A., Yen, H., White, M.J., Sheshukov, A.Y., Sadeghi, A.M., Moriasi, D.N., Steiner, J.L., Amatya, D.M., Skaggs, R.W. and Haney, E.B., (2015). Hydrological processes and model representation: impact of soft data on calibration. Trans. ASABE, 58(6):1637-1660.
Chauhan, P., Akıner, M.E., Sain, K. and Kumar, A., (2022). Forecasting of suspended sediment concentration in the Pindari-Kafni glacier valley in Central Himalayan region considering the impact of precipitation: using soft computing approach. Arab. J. Geosci., 15(8):683.
Chauhan, P., Sharma, J., Bhardwaj, P., Mehta, M., Shah, R.A., Singh, O. and Sain, K., (2023). Comparative analysis of discharge and sediment flux from two contiguous glacierized basins of Central Himalaya, India. Environ. Monit. Assess, 195(6):729.
Gassman, P.W., M. R. Reyes, C. H. Green, and J. G. Arnold. (2007). The Soil and Water Assessment Tool: Historical development, applications, and future research directions. Trans. ASABE, 50(4): 1211-1250. doi:10.13031/2013.23637.
Koltsida, E., Mamassis, N., and Kallioras, A. (2023). Hydrological modeling using the Soil and Water Assessment Tool in urban and peri-urban environments: the case of Kifisos experimental subbasin (Athens, Greece). Hydrol. Earth Syst. Sci., 27(4): 917-931.
Lizama, E., Somos-Valenzuela, M., Rivera, D., Lillo, M., Morales, B., Baraër, M. and Fernández, A., (2024). Role of mountain glaciers in the hydrological dynamics of headwater basins in the Wet Andes. J. Hydrol, 649:132413.
Londhe, D.S. and Katpatal, Y.B., (2020). Comparative assessment of evapotranspiration in Bhima sub-basin using spatial analysis for normal and ENSO years. J. Agrometeorol., 22(2): 179-185. https://doi.org/10.54386/jam.v22i2.159
Moriasi, D.N.; Arnold, J.G.; Van Liew, M.W.; Bingner, R.L.; Harmel, R.D.; Veith, T.L. (2007). Model Evaluation Guidelines for Systematic Quantification of Accuracy in Watershed Simulations. Trans. ASABE 50, 885–900.
Neitsch, S.L., Arnold, J.G., Kiniry, J.R. and Williams, J.R., (2011). Soil and water assessment tool theoretical documentation version 2009. Texas Water Resources Institute Technical report no. 406, Texas A&M University, Texas.
Padhiary, J., Patra, K.C., Das, D.M., Sahoo, B.C. and Singh, K.K., (2018). Prediction of climate change impact on streamflow and evapotranspiration in Baitarani basin using SWAT model. J. Agrometeorol., 20(4): 325-328. https://doi.org/10.54386/jam.v20i4.576
Rank, P.H., Vaghasiya, D.R., Lunagaria, M.M., Patel, R.J., Tiwari, M.K. and Rank, H.D., (2023). Climate change impacts on water flux dynamics in Shingoda basin having agriculture and forest ecosystems: A comprehensive analysis. J. Agrometeorol., 25(3): 397-403. https://doi.org/10.54386/jam.v25i3.2284
Singh, N., Singhal, M., Chhikara, S., Karakoti, I., Chauhan, P. and Dobhal, D.P., (2020). Radiation and energy balance dynamics over a rapidly receding glacier in the central Himalaya. Int. J. Climatol, 40(1):.400-420.
Singh, N., Bhattacharya, B. K., Soni, P., Raja, P., Singh, M.P. and Parihar, J. S., (2013). Energy and Water Dynamics Over Young Pine Forest as Influenced by Climatic Variability and Land Management Practices. J. Agrometeorol., 15(Special issue): 100-107.
Suryavanshi, S., Pandey, A., and Chaube, U. C. (2017). Hydrological simulation of the Betwa River basin (India) using the SWAT model. Hydrol. Sci. J., 62(6): 960-978.
Thakuri, S., and Salerno, F. (2016). Glacio-hydrological simulation in Dudh Koshi River basin, Nepal. Intern. J. Sci. Develop. Res. (IJSDR), 1:72-78.
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