Trend and change points of streamflow in the Yellow River and their attributions

The impacts of climate change and human activity, combined with streamflow reduction in the Yellow River Basin, have presented significant challenges to water resource management strategies. Here, the trends and change points of streamflow were determined for the period 1956–2017 via five statistica...

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Autores principales: Dunyu Zhong, Zengchuan Dong, Guobin Fu, Jiaqi Bian, Feihe Kong, Wenzhuo Wang, Yan Zhao
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Lenguaje:EN
Publicado: IWA Publishing 2021
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Acceso en línea:https://doaj.org/article/a6961a1169fb42ff97cb341c5084c99f
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spelling oai:doaj.org-article:a6961a1169fb42ff97cb341c5084c99f2021-11-05T18:40:53ZTrend and change points of streamflow in the Yellow River and their attributions2040-22442408-935410.2166/wcc.2020.144https://doaj.org/article/a6961a1169fb42ff97cb341c5084c99f2021-02-01T00:00:00Zhttp://jwcc.iwaponline.com/content/12/1/136https://doaj.org/toc/2040-2244https://doaj.org/toc/2408-9354The impacts of climate change and human activity, combined with streamflow reduction in the Yellow River Basin, have presented significant challenges to water resource management strategies. Here, the trends and change points of streamflow were determined for the period 1956–2017 via five statistical methods. A runoff-sensitive coefficients method (the Budyko hypothesis) and a conceptual rainfall–runoff model (the TUW model) were applied to assess the streamflow variation. The following conclusions were ascertained: (1) 1989, 1986, and 1990 were the change points for streamflow in the upstream Tang-Nai-Hai and Lan-Zhou stations and the downstream Hua-Yuan-Kou hydrological station; (2) the streamflow showed statistically significant decreasing trends with spatiotemporal variations in the Yellow River Basin; (3) the relationship between runoff and precipitation showed a downward trend over time; (4) comparisons of the Budyko and TUW models show that human activity is responsible for more than 65% of streamflow reduction, while climate change contributes to less than 35% of the reduction. Therefore, human activity is the main reason for streamflow reduction in the Yellow River Basin. This finding is of critical importance for water resources management under changing environment.Dunyu ZhongZengchuan DongGuobin FuJiaqi BianFeihe KongWenzhuo WangYan ZhaoIWA Publishingarticleclimate changehuman activitiesstreamflow variationyellow riverEnvironmental technology. Sanitary engineeringTD1-1066Environmental sciencesGE1-350ENJournal of Water and Climate Change, Vol 12, Iss 1, Pp 136-151 (2021)
institution DOAJ
collection DOAJ
language EN
topic climate change
human activities
streamflow variation
yellow river
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
spellingShingle climate change
human activities
streamflow variation
yellow river
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Dunyu Zhong
Zengchuan Dong
Guobin Fu
Jiaqi Bian
Feihe Kong
Wenzhuo Wang
Yan Zhao
Trend and change points of streamflow in the Yellow River and their attributions
description The impacts of climate change and human activity, combined with streamflow reduction in the Yellow River Basin, have presented significant challenges to water resource management strategies. Here, the trends and change points of streamflow were determined for the period 1956–2017 via five statistical methods. A runoff-sensitive coefficients method (the Budyko hypothesis) and a conceptual rainfall–runoff model (the TUW model) were applied to assess the streamflow variation. The following conclusions were ascertained: (1) 1989, 1986, and 1990 were the change points for streamflow in the upstream Tang-Nai-Hai and Lan-Zhou stations and the downstream Hua-Yuan-Kou hydrological station; (2) the streamflow showed statistically significant decreasing trends with spatiotemporal variations in the Yellow River Basin; (3) the relationship between runoff and precipitation showed a downward trend over time; (4) comparisons of the Budyko and TUW models show that human activity is responsible for more than 65% of streamflow reduction, while climate change contributes to less than 35% of the reduction. Therefore, human activity is the main reason for streamflow reduction in the Yellow River Basin. This finding is of critical importance for water resources management under changing environment.
format article
author Dunyu Zhong
Zengchuan Dong
Guobin Fu
Jiaqi Bian
Feihe Kong
Wenzhuo Wang
Yan Zhao
author_facet Dunyu Zhong
Zengchuan Dong
Guobin Fu
Jiaqi Bian
Feihe Kong
Wenzhuo Wang
Yan Zhao
author_sort Dunyu Zhong
title Trend and change points of streamflow in the Yellow River and their attributions
title_short Trend and change points of streamflow in the Yellow River and their attributions
title_full Trend and change points of streamflow in the Yellow River and their attributions
title_fullStr Trend and change points of streamflow in the Yellow River and their attributions
title_full_unstemmed Trend and change points of streamflow in the Yellow River and their attributions
title_sort trend and change points of streamflow in the yellow river and their attributions
publisher IWA Publishing
publishDate 2021
url https://doaj.org/article/a6961a1169fb42ff97cb341c5084c99f
work_keys_str_mv AT dunyuzhong trendandchangepointsofstreamflowintheyellowriverandtheirattributions
AT zengchuandong trendandchangepointsofstreamflowintheyellowriverandtheirattributions
AT guobinfu trendandchangepointsofstreamflowintheyellowriverandtheirattributions
AT jiaqibian trendandchangepointsofstreamflowintheyellowriverandtheirattributions
AT feihekong trendandchangepointsofstreamflowintheyellowriverandtheirattributions
AT wenzhuowang trendandchangepointsofstreamflowintheyellowriverandtheirattributions
AT yanzhao trendandchangepointsofstreamflowintheyellowriverandtheirattributions
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