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Snowmelt Runoff Simulation During Early 21st Century Using Hydrological Modelling in the Snow-Fed Terrain of Gilgit River Basin (Pakistan)

  • Yasir LatifEmail author
  • Yaoming Ma
  • Weiqiang Ma
  • Muhammad Sher
  • Yaseen Muhammad
Chapter
Part of the Advances in Science, Technology & Innovation book series (ASTI)

Abstract

The indispensable water supply of major reservoirs in Pakistan, essentially depends on meltwater runoff, mainly generating from the Upper Indus Basin (UIB). The present study includes snowmelt runoff simulation within Gilgit River, basin a sub basin of UIB. Snowmelt runoff model (SRM) incorporated with MODIS remote sensing snow cover products, was selected to simulate the daily discharges and to calculate the contribution of snowmelt impact on the discharge within Gilgit River basin, during the early 21st century (first decade). Our results revealed a Nash–Sutcliffe efficiency (NSE) as R2 (0.81) and average volume difference as DV (−0.51) in observed and simulated flow. Almost 9.2% of the total basin area is covered by glacier and permanent ice cover which contributes to the river runoff during summer. We also noted that the observed efficiency of the model becomes uncertain during high flow months such as June, July and August, such ambiguity during summer was attributed to glacier-melt runoff, which generates in August by the melting of glaciers.

Keywords

Runoff Gilgit river basin Climate change MODIS snow cover products SRM 

References

  1. 1.
    Adnan, M., Nabi, G., Saleem, P., Ashraf, A.: Snowmelt runoff prediction under changing climate in the Himalayan cryosphere: a case of Gilgit River Basin. Geosci. Front. 8, 941–947 (2016)CrossRefGoogle Scholar
  2. 2.
    Butt, M., Bilal, M.: Application of snowmelt runoff model for water resource management. Hydrological Process 25, 3735–3747 (2011)CrossRefGoogle Scholar
  3. 3.
    Hasson, S., Lucarini, V., Khan, M., Petitta, M., Bolch, T., Gioli, G.: Early 21st century Snow cover state over 5 the western river basins of the Indus River system. Hydrol. Earth Syst. Sci. 18, 4077–4100 (2014).  https://doi.org/10.5194/hess-18-4077-2014
  4. 4.
    Hasson, S., Böhner, J., Lucarini, V.: Prevailing climatic trends and runoff response from Hindukush–Karakoram–Himalaya, upper Indus basin. Earth Syst. Dyn. Discuss. 6, 579–653 (2015)CrossRefGoogle Scholar
  5. 5.
    Immerzeel, W., Droogers, P., De Jong, S.M., Bierkens, M.F.P.: Large-scale monitoring of snow cover and runoff simulation in Himalayan river basins using remote sensing. Remote Sens. Environ. 113, 40–49 (2009)CrossRefGoogle Scholar
  6. 6.
    Immerzeel, W.W., Van Beek, L.P.H., Bierkens, M.F.P.: Climate change will affect the Asian water towers. Science 328, 1382–1385 (2010)CrossRefGoogle Scholar
  7. 7.
    Immerzeel, W.W., Pellicciotti, F., Bierkens, M.F.P.: Rising river flows throughout the twenty-first century in two Himalayan glacierized watersheds. Nat. Geosci. 6, 742–745 (2013)CrossRefGoogle Scholar
  8. 8.
    Khan, A.: Hydrological modelling and their biases: constraints in policy making and sustainable water resources development under changing.climate in the Hindukush-Karakoram-Himalayas. Brief for GSDR (2015)Google Scholar
  9. 9.
    Latif, Y., Yaoming, M. and Yaseen, M.: Spatial nalysis of precipitation time series. Theor. Appl. Climatol. 131, 761–775 (2016).  https://doi.org/10.1007/s00704-016-2007-3
  10. 10.
    Martinec, J.: Snowmelt-Runoff model for stream flow forecasts. Nord. Hydrol. 6, 145–154 (1975)CrossRefGoogle Scholar
  11. 11.
    Minora, U., Bocchiola, D., D’Agata C., Maragno, D., Mayer, C., Lambrecht, A., Mosconi, B., Vuillermoz, E., Senese, A., Compostella, C., Smiraglia, C., and Diolaiuti, G.: 2001–2010 glacier changes in the Central Karakoram National Park: a contribution to evaluate the magnitude and rate of the “Karakoram anomaly”. Cryosphere Discuss. 7, 2891–2941(2013)Google Scholar
  12. 12.
    Mukhopadhyaya, B., Khan, A.: Rising river flows and glacial mass balance in central Karakoram. J. Hydrol. 513, 192–203 (2014)CrossRefGoogle Scholar
  13. 13.
    Tahir, A., Chevallier, P., Arnaud, Y., Neppel, L., Ahmad, B.: Modeling snowmelt-runoff under climate change scenarios in the Hunza River basin, Karakoram Range, Northern Pakistan. J. Hydrol. 409, 104–111 (2011)CrossRefGoogle Scholar
  14. 14.
    Tahir, A.A., Chevallier, P., Arnaud, Y., Ashraf, M., & Bhatti, M.T.: Snow cover trend and hydrological characteristics of the Astore River basin (Western Himalayas) and its comparison to the Hunza basin (Karakoram region). Sci Total Environ. 505, 748–761 (2015)Google Scholar

Copyright information

© Springer Nature Switzerland AG 2019

Authors and Affiliations

  • Yasir Latif
    • 1
    • 3
    • 5
    Email author
  • Yaoming Ma
    • 1
    • 2
    • 3
  • Weiqiang Ma
    • 1
    • 3
  • Muhammad Sher
    • 4
  • Yaseen Muhammad
    • 6
  1. 1.Key Laboratory of Tibetan Environment Changes and Land Surface ProcessesInstitute of Tibetan Plateau Research, Chinese Academy of SciencesBeijingChina
  2. 2.CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of SciencesBeijingChina
  3. 3.University of Chinese Academy of SciencesBeijingChina
  4. 4.Institite of International Rivers and ECO-Security, Yunnan UniversityKunmingChina
  5. 5.University of Agriculture FaisalabadFaisalabadPakistan
  6. 6.Centre for Integrated Mountain Research, University of the PunjabLahorePakistan

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