Modelling climate change impact on water resources of the Upper Indus Basin

Jamal H. Ougahi (Lead / Corresponding author), Mark E. J. Cutler, Simon J. Cook

    Research output: Contribution to journalArticlepeer-review

    6 Citations (Scopus)
    51 Downloads (Pure)

    Abstract

    Climate change has implications for water resources by increasing temperature, shifting precipitation patterns and altering the timing of snowfall and glacier melt, leading to shifts in the seasonality of river flows. Here, the Soil & Water Assessment Tool was run using downscaled precipitation and temperature projections from five global climate models (GCMs) and their multi-model mean to estimate the potential impact of climate change on water balance components in sub-basins of the Upper Indus Basin (UIB) under two emission (RCP4.5 and RCP8.5) and future (2020–2050 and 2070–2100) scenarios. Warming of above 6 °C relative to baseline (1974–2004) is projected for the UIB by the end of the century (2070–2100), but the spread of annual precipitation projections among GCMs is large (þ16 to 28%), and even larger for seasonal precipitation (þ91 to 48%). Compared to the baseline, an increase in summer precipitation (RCP8.5: þ36.7%) and a decrease in winter precipitation were projected (RCP8.5: 16.9%), with an increase in average annual water yield from the nival–glacial regime and river flow peaking 1 month earlier. We conclude that predicted warming during winter and spring could substantially affect the seasonal river flows, with important implications for water supplies.

    Original languageEnglish
    Pages (from-to)482-504
    Number of pages23
    JournalJournal of Water and Climate Change
    Volume13
    Issue number2
    Early online date29 Nov 2021
    DOIs
    Publication statusPublished - 1 Feb 2022

    Keywords

    • climate change
    • GCMs
    • precipitation
    • SWAT
    • temperature
    • water balance

    Fingerprint

    Dive into the research topics of 'Modelling climate change impact on water resources of the Upper Indus Basin'. Together they form a unique fingerprint.

    Cite this