Contemporary Trends in High and Low River Flows in Upper Indus Basin, Pakistan

0553293 - ÚI 2023 RIV CH eng J - Článek v odborném periodiku
Yaseen, M. - Latif, Yasir - Waseem, M. - Leta, M. K. - Abbas, S. - Bhatti, H. A.
Contemporary Trends in High and Low River Flows in Upper Indus Basin, Pakistan.
Water. Roč. 14, č. 3 (2022), č. článku 337. E-ISSN 2073-4441
Institucionální podpora: RVO:67985807
Klíčová slova: Upper Indus Basin * streamflows * flow extremes * high and low flows * Mann-Kendall * Jhelum River basin * Kabul River basin * significant trends * climate change
Obor OECD: Hydrology
Impakt faktor: 3.4, rok: 2022
Způsob publikování: Open access
http://dx.doi.org/10.3390/w14030337

The Upper Indus Basin (UIB) features the high mountain ranges of the Hindukush, Karakoram and Himalaya (HKH). The snow and glacier meltwater contribution feeds 10 major river basins downstream including Astore, Gilgit, Hunza, Jhelum, Kabul, Shyok and Shigar. Climate change is likely to fluctuate the runoff generated from such river basins concerning high and low streamflows. Widening the lens of focus, the present study examines the magnitude and timing of high flows variability as well as trends variability in low streamflows using Sen’s slope and the Mann-Kendall test in UIB from 1981 to 2016. The results revealed that the trend in the magnitude of the high flows decreased at most of the sub-basins including the Jhelum, Indus and Kabul River basins. Significantly increased high flows were observed in the glacier regime of UIB at Shigar and Shyok while decreased flows were predominant in Hunza River at Daniyor Bridge. A similar proclivity of predominantly reduced flows was observed in nival and rainfall regimes in terms of significant negative trends in the Jhelum, Kunhar, Neelum and Poonch River basins. The timing of the high flows has not changed radically as magnitude at all gauging stations. For the low flows, decreasing significant trends were detected in the annual flows as well as in other extremes of low flows (1-day, 7-day, 15-day). The more profound and decreasing pattern of low flows was observed in summer at most of the gauging stations. However, such stations exhibited increased low flows in autumn, winter and spring. The decrease in low flows indicates the extension of dry periods particularly in summer. The high-water demand in summer will be compromised due to consistently reducing summer flows. The lower the water availability, the lower will be the crop yield and electricity generation.
Trvalý link: http://hdl.handle.net/11104/0328272