Assessing the impact of climate variability and human activities on streamflow variation

Water resources in river systems have been changing under the impact of both climate variability and human activities. Assessing the respective impact on decadal streamflow variation is important for water resource management. By using an elasticity-based method and calibrated TOPMODEL and VIC hydro...

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Main Authors: J. Chang, H. Zhang, Y. Wang, Y. Zhu
Format: Article
Language:English
Published: Copernicus Publications 2016-04-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/20/1547/2016/hess-20-1547-2016.pdf
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spelling doaj-85ff292d0f8148d28b8dc1b5bc40d1e22020-11-24T21:06:50ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382016-04-012041547156010.5194/hess-20-1547-2016Assessing the impact of climate variability and human activities on streamflow variationJ. Chang0H. Zhang1Y. Wang2Y. Zhu3State Key Laboratory Base of Eco-hydraulic Engineering in Arid Area, Xi'an University of Technology, Xi'an 710048, ChinaState Key Laboratory Base of Eco-hydraulic Engineering in Arid Area, Xi'an University of Technology, Xi'an 710048, ChinaState Key Laboratory Base of Eco-hydraulic Engineering in Arid Area, Xi'an University of Technology, Xi'an 710048, ChinaState Key Laboratory Base of Eco-hydraulic Engineering in Arid Area, Xi'an University of Technology, Xi'an 710048, ChinaWater resources in river systems have been changing under the impact of both climate variability and human activities. Assessing the respective impact on decadal streamflow variation is important for water resource management. By using an elasticity-based method and calibrated TOPMODEL and VIC hydrological models, we quantitatively isolated the relative contributions that human activities and climate variability made to decadal streamflow changes in the Jinghe basin, located in the northwest of China. This is an important watershed of the Shaanxi province that supplies drinking water for a population of over 6 million people. The results showed that the maximum value of the moisture index (<i>E</i><sub>0</sub>∕<i>P</i>) was 1.91 and appeared in 1991&ndash;2000, and the decreased speed of streamflow was higher since 1990 compared with 1960&ndash;1990. The average annual streamflow from 1990 to 2010 was reduced by 26.96 % compared with the multiyear average value (from 1960 to 2010). The estimates of the impacts of climate variability and human activities on streamflow decreases from the hydrological models were similar to those from the elasticity-based method. The maximum contribution value of human activities was 99 % when averaged over the three methods, and appeared in 1981&ndash;1990 due to the effects of soil and water conservation measures and irrigation water withdrawal. Climate variability made the greatest contribution to streamflow reduction in 1991&ndash;2000, the values of which was 40.4 %. We emphasized various source of errors and uncertainties that may occur in the hydrological model (parameter and structural uncertainty) and elasticity-based method (model parameter) in climate change impact studies.http://www.hydrol-earth-syst-sci.net/20/1547/2016/hess-20-1547-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. Chang
H. Zhang
Y. Wang
Y. Zhu
spellingShingle J. Chang
H. Zhang
Y. Wang
Y. Zhu
Assessing the impact of climate variability and human activities on streamflow variation
Hydrology and Earth System Sciences
author_facet J. Chang
H. Zhang
Y. Wang
Y. Zhu
author_sort J. Chang
title Assessing the impact of climate variability and human activities on streamflow variation
title_short Assessing the impact of climate variability and human activities on streamflow variation
title_full Assessing the impact of climate variability and human activities on streamflow variation
title_fullStr Assessing the impact of climate variability and human activities on streamflow variation
title_full_unstemmed Assessing the impact of climate variability and human activities on streamflow variation
title_sort assessing the impact of climate variability and human activities on streamflow variation
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2016-04-01
description Water resources in river systems have been changing under the impact of both climate variability and human activities. Assessing the respective impact on decadal streamflow variation is important for water resource management. By using an elasticity-based method and calibrated TOPMODEL and VIC hydrological models, we quantitatively isolated the relative contributions that human activities and climate variability made to decadal streamflow changes in the Jinghe basin, located in the northwest of China. This is an important watershed of the Shaanxi province that supplies drinking water for a population of over 6 million people. The results showed that the maximum value of the moisture index (<i>E</i><sub>0</sub>∕<i>P</i>) was 1.91 and appeared in 1991&ndash;2000, and the decreased speed of streamflow was higher since 1990 compared with 1960&ndash;1990. The average annual streamflow from 1990 to 2010 was reduced by 26.96 % compared with the multiyear average value (from 1960 to 2010). The estimates of the impacts of climate variability and human activities on streamflow decreases from the hydrological models were similar to those from the elasticity-based method. The maximum contribution value of human activities was 99 % when averaged over the three methods, and appeared in 1981&ndash;1990 due to the effects of soil and water conservation measures and irrigation water withdrawal. Climate variability made the greatest contribution to streamflow reduction in 1991&ndash;2000, the values of which was 40.4 %. We emphasized various source of errors and uncertainties that may occur in the hydrological model (parameter and structural uncertainty) and elasticity-based method (model parameter) in climate change impact studies.
url http://www.hydrol-earth-syst-sci.net/20/1547/2016/hess-20-1547-2016.pdf
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