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Estimation of component-wise runoff contribution using temperature index approach, in a snow- and glacier-fed transboundary Shyok River catchment of the Upper Indus Basin

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Abstract

The study is focused on the estimation of component-wise runoff using temperature-index approach for the snow and glacier dominated Shyok River catchment; a sub-basin of the Upper Indus basin (UIB). Shyok River is a transboundary stream that has a catchment area of 33,465 km2 over three countries; Pakistan 28%, India 54%, and China 18%. To achieve the objective of the study, temperature-index approach-based snow and glacier melt runoff model (SRM+G) was applied in the Shyok River catchment for the duration of 2003–2014. The satellite-based remote-sensed MODIS snow-covered area (MOD10A1.005), NOAA RFE CA 2.0 precipitation and Landsat8 scenes’ extracted glacier extent were used in the model at daily time scale. SRTM 90m DEM was used for the catchment processing and its division into particular elevation zones in view of the modelling requirements. Based on the ground-observed temperature data of stations across UIB, an equation was developed using regression analysis for the estimation of temperature lapse rate (TLR) in the region. The daily temperature records at Hushey stations were projected for the constructed elevations zones using the estimated TLR of 0.64 °C per 100 m. The model was calibrated and validated using the daily streamflow record of Shyok River at Yogo station with a mean coefficient of determination (R2) of 0.93. An acceptable agreement of ± 10% error was achieved for the simulated annual inflow volume except for year 2010 that carried a rainfall-generated flood in summer season. The mean annual contribution from glacier melt, snowmelt and rainfall was estimated as 49%, 39% and 12%, respectively. The glacier melt was found to be the dominant contributor in the annual inflow. Snow-covered and glacier-exposed map** of the catchment was also carried out on long-term monthly basis. The findings of the study are beneficial for the water resources managers in the concerned organisations for the improved flow forecasting and water resources management in the region.

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Data Availability

The data can be requested from SWHP-WAPDA and PMD Pakistan.

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Acknowledgements

The authors acknowledge the Surface Water Hydrology Project, Glacier Monitoring Research Centre, Water and Power Development Authority, Pakistan Meteorological Department, International Centre for Tropical Agriculture, National Oceanic Atmospheric Administration, National Aeronautics and Space Administration and the United States Geological Survey for making possible the availability of required data to coagulate this research work. The author also acknowledges the assistance of Mr. Adil Latif, GIS Expert NESPAK.

Funding

This was self-funded research. It was carried out as part of the degree requirement for the Masters’s program in Hydraulics and Irrigation Engineering at the University of Engineering and Technology Lahore, Pakistan.

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Muhammad Umar Farooq and Dr. Muhammad Ashiq Kharal designed the research plan. Muhammad Umar Farooq and Muhammad Fraz Ismail performed the analysis and interpreted the results. Asif Mehmood contributed in the discussions. Dr. Wolfgang Bogacki supervised the research. He also provided valuable suggestions for the improvement of the article. All authors read and approved the final manuscript.

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Correspondence to Muhammad Umar Farooq.

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Farooq, M.U., Kharal, M.A., Bogacki, W. et al. Estimation of component-wise runoff contribution using temperature index approach, in a snow- and glacier-fed transboundary Shyok River catchment of the Upper Indus Basin. Arab J Geosci 16, 460 (2023). https://doi.org/10.1007/s12517-023-11583-y

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