Understanding Future Water Challenges in a Highly Regulated Indian River Basin—Modelling the Impact of Climate Change on the Hydrology of the Upper Narmada
Nathan Rickards,
Thomas Thomas,
Alexandra Kaelin,
Helen Houghton-Carr,
Sharad K. Jain,
Prabhash K. Mishra,
Manish K. Nema,
Harry Dixon,
Mohammed M. Rahman,
Robyn Horan,
Alan Jenkins,
Gwyn Rees
Affiliations
Nathan Rickards
UK Centre for Ecology & Hydrology, Wallingford OX10 8BB, UK
Thomas Thomas
National Institute of Hydrology, Roorkee 247667, India
Alexandra Kaelin
UK Centre for Ecology & Hydrology, Wallingford OX10 8BB, UK
Helen Houghton-Carr
UK Centre for Ecology & Hydrology, Wallingford OX10 8BB, UK
Sharad K. Jain
National Institute of Hydrology, Roorkee 247667, India
Prabhash K. Mishra
National Institute of Hydrology, Roorkee 247667, India
Manish K. Nema
National Institute of Hydrology, Roorkee 247667, India
Harry Dixon
UK Centre for Ecology & Hydrology, Wallingford OX10 8BB, UK
Mohammed M. Rahman
Department of Irrigation and Water Management, Bangladesh Agricultural University, Mymensingh 2202, Bangladesh
Robyn Horan
UK Centre for Ecology & Hydrology, Wallingford OX10 8BB, UK
Alan Jenkins
UK Centre for Ecology & Hydrology, Wallingford OX10 8BB, UK
Gwyn Rees
UK Centre for Ecology & Hydrology, Wallingford OX10 8BB, UK
The Narmada river basin is a highly regulated catchment in central India, supporting a population of over 16 million people. In such extensively modified hydrological systems, the influence of anthropogenic alterations is often underrepresented or excluded entirely by large-scale hydrological models. The Global Water Availability Assessment (GWAVA) model is applied to the Upper Narmada, with all major dams, water abstractions and irrigation command areas included, which allows for the development of a holistic methodology for the assessment of water resources in the basin. The model is driven with 17 Global Circulation Models (GCMs) from the Coupled Model Intercomparison Project Phase 5 (CMIP5) ensemble to assess the impact of climate change on water resources in the basin for the period 2031–2060. The study finds that the hydrological regime within the basin is likely to intensify over the next half-century as a result of future climate change, causing long-term increases in monsoon season flow across the Upper Narmada. Climate is expected to have little impact on dry season flows, in comparison to water demand intensification over the same period, which may lead to increased water stress in parts of the basin.