Modified hydrologic regime of upper Ganga basin induced by natural and anthropogenic stressors

Abstract Climate change and anthropogenic activities pose serious threats to river basin hydrology worldwide. The Ganga basin is home to around half a billion people and has been significantly impacted by hydrological alterations in the last few decades. The increasing high-intensity rainfall events...

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Main Authors: Somil Swarnkar, Pradeep Mujumdar, Rajiv Sinha
Format: Article
Language:English
Published: Nature Publishing Group 2021-09-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-98827-7
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spelling doaj-69c7e5108b8c4440ab91a35a3b78c3fe2021-10-03T11:29:44ZengNature Publishing GroupScientific Reports2045-23222021-09-0111111110.1038/s41598-021-98827-7Modified hydrologic regime of upper Ganga basin induced by natural and anthropogenic stressorsSomil Swarnkar0Pradeep Mujumdar1Rajiv Sinha2Interdisciplinary Centre for Water and Research (ICWaR), Indian Institute of Science (IISc)Interdisciplinary Centre for Water and Research (ICWaR), Indian Institute of Science (IISc)Department of Earth Sciences, Indian Institute of Technology Kanpur (IITK)Abstract Climate change and anthropogenic activities pose serious threats to river basin hydrology worldwide. The Ganga basin is home to around half a billion people and has been significantly impacted by hydrological alterations in the last few decades. The increasing high-intensity rainfall events often create flash flooding events. Such events are frequently reported in mountainous and alluvial plains of the Ganga basin, putting the entire basin under severe flood risk. Further, increasing human interventions through hydraulic structures in the upstream reaches significantly alter the flows during the pre-and post-monsoon periods. Here, we explore the hydrological implications of increasing reservoir-induced and climate-related stressors in the Upper Ganga Basin (UGB), India. Flow/sediment duration curves and flood frequency analysis have been used to assess pre-and post-1995 hydrological behaviour. Our results indicate that low and moderate flows have been significantly altered, and the flood peaks have been attenuated by the operation of hydraulic structures in the Bhagirathi (western subbasin). The Alaknanda (eastern subbasin) has experienced an increase in extreme rainfall and flows post-1995. The downstream reaches experience reservoir-induced moderate flow alterations during pre-and post-monsoon and increasing extreme flood magnitudes during monsoon. Furthermore, substantial siltation upstream of the reservoirs has disrupted the upstream–downstream geomorphologic linkages.https://doi.org/10.1038/s41598-021-98827-7
collection DOAJ
language English
format Article
sources DOAJ
author Somil Swarnkar
Pradeep Mujumdar
Rajiv Sinha
spellingShingle Somil Swarnkar
Pradeep Mujumdar
Rajiv Sinha
Modified hydrologic regime of upper Ganga basin induced by natural and anthropogenic stressors
Scientific Reports
author_facet Somil Swarnkar
Pradeep Mujumdar
Rajiv Sinha
author_sort Somil Swarnkar
title Modified hydrologic regime of upper Ganga basin induced by natural and anthropogenic stressors
title_short Modified hydrologic regime of upper Ganga basin induced by natural and anthropogenic stressors
title_full Modified hydrologic regime of upper Ganga basin induced by natural and anthropogenic stressors
title_fullStr Modified hydrologic regime of upper Ganga basin induced by natural and anthropogenic stressors
title_full_unstemmed Modified hydrologic regime of upper Ganga basin induced by natural and anthropogenic stressors
title_sort modified hydrologic regime of upper ganga basin induced by natural and anthropogenic stressors
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2021-09-01
description Abstract Climate change and anthropogenic activities pose serious threats to river basin hydrology worldwide. The Ganga basin is home to around half a billion people and has been significantly impacted by hydrological alterations in the last few decades. The increasing high-intensity rainfall events often create flash flooding events. Such events are frequently reported in mountainous and alluvial plains of the Ganga basin, putting the entire basin under severe flood risk. Further, increasing human interventions through hydraulic structures in the upstream reaches significantly alter the flows during the pre-and post-monsoon periods. Here, we explore the hydrological implications of increasing reservoir-induced and climate-related stressors in the Upper Ganga Basin (UGB), India. Flow/sediment duration curves and flood frequency analysis have been used to assess pre-and post-1995 hydrological behaviour. Our results indicate that low and moderate flows have been significantly altered, and the flood peaks have been attenuated by the operation of hydraulic structures in the Bhagirathi (western subbasin). The Alaknanda (eastern subbasin) has experienced an increase in extreme rainfall and flows post-1995. The downstream reaches experience reservoir-induced moderate flow alterations during pre-and post-monsoon and increasing extreme flood magnitudes during monsoon. Furthermore, substantial siltation upstream of the reservoirs has disrupted the upstream–downstream geomorphologic linkages.
url https://doi.org/10.1038/s41598-021-98827-7
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