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Water availability and response of Tarbela Reservoir under the changing climate in the Upper Indus Basin, Pakistan
Agriculture is one of the major contributors to the Gross Domestic Product (GDP) of Pakistan which relies on the availability of water. Hydropower contributes approximately 35% to the national electricity gid of Pakistan. Indus River is the main river of the Indus River System (IRS) which provides w...
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2022
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9508107/ https://www.ncbi.nlm.nih.gov/pubmed/36151258 http://dx.doi.org/10.1038/s41598-022-20159-x |
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author | Khan, Firdos |
author_facet | Khan, Firdos |
author_sort | Khan, Firdos |
collection | PubMed |
description | Agriculture is one of the major contributors to the Gross Domestic Product (GDP) of Pakistan which relies on the availability of water. Hydropower contributes approximately 35% to the national electricity gid of Pakistan. Indus River is the main river of the Indus River System (IRS) which provides water for agriculture, hydropower and other purposes. The outputs of the Conformal-Cubic Atmospheric Model (CCAM) are used to force the University of British Columbia Watershed Model (UBCWM) in the Upper Indus Basin (UIB), to investigate future water availability under the two IPCC emission scenarios (RCP4.5 and RCP8.5). Tarbela Reservoir which is the outlet of UIB is used as a measurement tool to assess water availability and response of the reservoir to climate change. The results show that maximum and minimum temperature are increasing in the future in comparison to the reference period. The largest increases in maximum temperature are projected for MAM (March–April–May) and JJA (June–July–August), with increases up to 2 °C in MAM and increases up to 6.4 °C in JJA under the RCP4.5 and RCP8.5, respectively, in the future. Minimum temperature has maximum increase (6.7 °C) in DJF (December–January–February) during 2071–2100 under RCP8.5. Precipitation shows a 5.1% decrease in DJF during 2011–2040 under RCP4.5. The statistics about water availability suggest that there is consistent increase in most of the months in the future, however, under the RCP4.5, there is decline in the river flow during 2071–2100 as compared to the 2041–2070. The findings of this study show that most of the time there will be more water available but in some months, there may be water scarcity under the RCP4.5, however, proper management and optimal utilization can reduce the water scarcity. |
format | Online Article Text |
id | pubmed-9508107 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-95081072022-09-25 Water availability and response of Tarbela Reservoir under the changing climate in the Upper Indus Basin, Pakistan Khan, Firdos Sci Rep Article Agriculture is one of the major contributors to the Gross Domestic Product (GDP) of Pakistan which relies on the availability of water. Hydropower contributes approximately 35% to the national electricity gid of Pakistan. Indus River is the main river of the Indus River System (IRS) which provides water for agriculture, hydropower and other purposes. The outputs of the Conformal-Cubic Atmospheric Model (CCAM) are used to force the University of British Columbia Watershed Model (UBCWM) in the Upper Indus Basin (UIB), to investigate future water availability under the two IPCC emission scenarios (RCP4.5 and RCP8.5). Tarbela Reservoir which is the outlet of UIB is used as a measurement tool to assess water availability and response of the reservoir to climate change. The results show that maximum and minimum temperature are increasing in the future in comparison to the reference period. The largest increases in maximum temperature are projected for MAM (March–April–May) and JJA (June–July–August), with increases up to 2 °C in MAM and increases up to 6.4 °C in JJA under the RCP4.5 and RCP8.5, respectively, in the future. Minimum temperature has maximum increase (6.7 °C) in DJF (December–January–February) during 2071–2100 under RCP8.5. Precipitation shows a 5.1% decrease in DJF during 2011–2040 under RCP4.5. The statistics about water availability suggest that there is consistent increase in most of the months in the future, however, under the RCP4.5, there is decline in the river flow during 2071–2100 as compared to the 2041–2070. The findings of this study show that most of the time there will be more water available but in some months, there may be water scarcity under the RCP4.5, however, proper management and optimal utilization can reduce the water scarcity. Nature Publishing Group UK 2022-09-23 /pmc/articles/PMC9508107/ /pubmed/36151258 http://dx.doi.org/10.1038/s41598-022-20159-x Text en © The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Article Khan, Firdos Water availability and response of Tarbela Reservoir under the changing climate in the Upper Indus Basin, Pakistan |
title | Water availability and response of Tarbela Reservoir under the changing climate in the Upper Indus Basin, Pakistan |
title_full | Water availability and response of Tarbela Reservoir under the changing climate in the Upper Indus Basin, Pakistan |
title_fullStr | Water availability and response of Tarbela Reservoir under the changing climate in the Upper Indus Basin, Pakistan |
title_full_unstemmed | Water availability and response of Tarbela Reservoir under the changing climate in the Upper Indus Basin, Pakistan |
title_short | Water availability and response of Tarbela Reservoir under the changing climate in the Upper Indus Basin, Pakistan |
title_sort | water availability and response of tarbela reservoir under the changing climate in the upper indus basin, pakistan |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9508107/ https://www.ncbi.nlm.nih.gov/pubmed/36151258 http://dx.doi.org/10.1038/s41598-022-20159-x |
work_keys_str_mv | AT khanfirdos wateravailabilityandresponseoftarbelareservoirunderthechangingclimateintheupperindusbasinpakistan |