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Assessment of Spatial and Temporal Flow Variability of the Indus River

Author

Listed:
  • Muhammad Arfan

    (USPCAS-W, MUET Sindh, Jamshoro 76090, Pakistan)

  • Jewell Lund

    (Department of Geography, University of Utah, Salt Lake City, UT 84112, USA)

  • Daniyal Hassan

    (Department of Civil & Environmental Engineering, University of Utah, Salt Lake City, UT 84112, USA)

  • Maaz Saleem

    (USPCAS-W, MUET Sindh, Jamshoro 76090, Pakistan)

  • Aftab Ahmad

    (USPCAS-W, MUET Sindh, Jamshoro 76090, Pakistan)

Abstract

Considerable controversy exists among researchers over the behavior of glaciers in the Upper Indus Basin (UIB) with regard to climate change. Glacier monitoring studies using the Geographic Information System (GIS) and remote sensing techniques have given rise to contradictory results for various reasons. This uncertain situation deserves a thorough examination of the statistical trends of temperature and streamflow at several gauging stations, rather than relying solely on climate projections. Planning for equitable distribution of water among provinces in Pakistan requires accurate estimation of future water resources under changing flow regimes. Due to climate change, hydrological parameters are changing significantly; consequently the pattern of flows are changing. The present study assesses spatial and temporal flow variability and identifies drought and flood periods using flow data from the Indus River. Trends and variations in river flows were investigated by applying the Mann-Kendall test and Sen’s method. We divide the annual water cycle into two six-month and four three-month seasons based on the local water cycle pattern. A decile indices technique is used to determine drought and flood periods. Overall, the analysis indicates that flow and temperature variabilities are greater seasonally than annually. At the Tarbela Dam, Indus River, annual mean, maximum, and minimum flows decreased steeply from 1986–2010 compared to the 1961–1985 period. Seasonal flow analysis unveils a more complex flow regime: Winter (October–March), (December–February), and spring (March–May) seasons demonstrate increasing flows along with increasing maximum temperature, whereas summer (April–September), (June–August) and autumn (September–November) showed decreasing trends in the flow. Spatial analysis shows that minimum discharge increased at the higher elevation gauging station (Kharmong, 2542 m.a.s.l.) and decreased at the lower elevation gauging station (Tarbela). Over the same timeframe, maximum and mean discharges decreased more substantially at lower elevations than at higher elevations. Drought and flood analysis revealed 2000–2004 to be the driest period in the Indus Basin for this record.

Suggested Citation

  • Muhammad Arfan & Jewell Lund & Daniyal Hassan & Maaz Saleem & Aftab Ahmad, 2019. "Assessment of Spatial and Temporal Flow Variability of the Indus River," Resources, MDPI, vol. 8(2), pages 1-17, May.
    • Handle: RePEc:gam:jresou:v:8:y:2019:i:2:p:103-:d:235967
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    References listed on IDEAS

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    3. Jane Qiu, 2008. "China: The third pole," Nature, Nature, vol. 454(7203), pages 393-396, July.
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    Cited by:

    1. Muhammad Shehzad Ashraf & Muhammad Shahid & Muhammad Waseem & Muhammad Azam & Khalil Ur Rahman, 2023. "Assessment of Variability in Hydrological Droughts Using the Improved Innovative Trend Analysis Method," Sustainability, MDPI, vol. 15(11), pages 1-20, June.
    2. Maaz Saleem & Muhammad Arfan & Kamran Ansari & Daniyal Hassan, 2023. "Analyzing the Impact of Ungauged Hill Torrents on the Riverine Floods of the River Indus: A Case Study of Koh E Suleiman Mountains in the DG Khan and Rajanpur Districts of Pakistan," Resources, MDPI, vol. 12(2), pages 1-18, February.

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