Hydrological response to climate change and human activities: A case study of Taihu Basin, China

Climate change and human activities have changed a number of characteristics of river flow in the Taihu Basin. Based on long-term time series of hydrological data from 1986 to 2015, we analyzed variability in precipitation, water stage, water diversion from the Yangtze River, and net inflow into Tai...

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Main Authors: Juan Wu, Zhi-yong Wu, He-juan Lin, Hai-ping Ji, Min Liu
Format: Article
Language:English
Published: Elsevier 2020-06-01
Series:Water Science and Engineering
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674237020300521
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spelling doaj-410bfd847cb44a9f826de799520b87a52020-11-25T03:20:48ZengElsevierWater Science and Engineering1674-23702020-06-011328394Hydrological response to climate change and human activities: A case study of Taihu Basin, ChinaJuan Wu0Zhi-yong Wu1He-juan Lin2Hai-ping Ji3Min Liu4Bureau of Hydrology, Taihu Basin Authority of Ministry of Water Resources, Shanghai 200434, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, China; Corresponding author.Bureau of Hydrology, Taihu Basin Authority of Ministry of Water Resources, Shanghai 200434, ChinaBureau of Hydrology, Taihu Basin Authority of Ministry of Water Resources, Shanghai 200434, ChinaBureau of Hydrology, Taihu Basin Authority of Ministry of Water Resources, Shanghai 200434, ChinaClimate change and human activities have changed a number of characteristics of river flow in the Taihu Basin. Based on long-term time series of hydrological data from 1986 to 2015, we analyzed variability in precipitation, water stage, water diversion from the Yangtze River, and net inflow into Taihu Lake with the Mann-Kendall test. The non-stationary relationship between precipitation and water stage was first analyzed for the Taihu Basin and the Wuchengxiyu (WCXY) sub-region. The optimized regional and urban regulation schemes were explored to tackle high water stage problems through the hydrodynamic model. The results showed the following: (1) The highest, lowest, and average Taihu Lake water stages of all months had increasing trends. The total net inflow into Taihu Lake from the Huxi (HX) sub-region and the Wangting Sluice increased significantly. (2) The Taihu Lake water stage decreased much more slowly after 2002; it was steadier and higher after 2002. After the construction of Wuxi urban flood control projects, the average water stage of the inner city was 0.16–0.40 m lower than that of suburbs in the flood season, leading to the transfer of flooding in inner cities to suburbs and increasing inflow from HX into Taihu Lake. (3) The regional optimized schemes were more satisfactory in not increasing the inner city flood control burden, thereby decreasing the average water stage by 0.04–0.13 m, and the highest water stage by 0.04–0.09 m for Taihu Lake and the sub-region in the flood season. Future flood control research should set the basin as the basic unit. Decreasing diversion and drainage lines along the Yangtze River can take an active role in flood control.http://www.sciencedirect.com/science/article/pii/S1674237020300521Hydrological responseClimate changeHuman activitiesFlood controlMann-Kendall testTaihu Basin
collection DOAJ
language English
format Article
sources DOAJ
author Juan Wu
Zhi-yong Wu
He-juan Lin
Hai-ping Ji
Min Liu
spellingShingle Juan Wu
Zhi-yong Wu
He-juan Lin
Hai-ping Ji
Min Liu
Hydrological response to climate change and human activities: A case study of Taihu Basin, China
Water Science and Engineering
Hydrological response
Climate change
Human activities
Flood control
Mann-Kendall test
Taihu Basin
author_facet Juan Wu
Zhi-yong Wu
He-juan Lin
Hai-ping Ji
Min Liu
author_sort Juan Wu
title Hydrological response to climate change and human activities: A case study of Taihu Basin, China
title_short Hydrological response to climate change and human activities: A case study of Taihu Basin, China
title_full Hydrological response to climate change and human activities: A case study of Taihu Basin, China
title_fullStr Hydrological response to climate change and human activities: A case study of Taihu Basin, China
title_full_unstemmed Hydrological response to climate change and human activities: A case study of Taihu Basin, China
title_sort hydrological response to climate change and human activities: a case study of taihu basin, china
publisher Elsevier
series Water Science and Engineering
issn 1674-2370
publishDate 2020-06-01
description Climate change and human activities have changed a number of characteristics of river flow in the Taihu Basin. Based on long-term time series of hydrological data from 1986 to 2015, we analyzed variability in precipitation, water stage, water diversion from the Yangtze River, and net inflow into Taihu Lake with the Mann-Kendall test. The non-stationary relationship between precipitation and water stage was first analyzed for the Taihu Basin and the Wuchengxiyu (WCXY) sub-region. The optimized regional and urban regulation schemes were explored to tackle high water stage problems through the hydrodynamic model. The results showed the following: (1) The highest, lowest, and average Taihu Lake water stages of all months had increasing trends. The total net inflow into Taihu Lake from the Huxi (HX) sub-region and the Wangting Sluice increased significantly. (2) The Taihu Lake water stage decreased much more slowly after 2002; it was steadier and higher after 2002. After the construction of Wuxi urban flood control projects, the average water stage of the inner city was 0.16–0.40 m lower than that of suburbs in the flood season, leading to the transfer of flooding in inner cities to suburbs and increasing inflow from HX into Taihu Lake. (3) The regional optimized schemes were more satisfactory in not increasing the inner city flood control burden, thereby decreasing the average water stage by 0.04–0.13 m, and the highest water stage by 0.04–0.09 m for Taihu Lake and the sub-region in the flood season. Future flood control research should set the basin as the basic unit. Decreasing diversion and drainage lines along the Yangtze River can take an active role in flood control.
topic Hydrological response
Climate change
Human activities
Flood control
Mann-Kendall test
Taihu Basin
url http://www.sciencedirect.com/science/article/pii/S1674237020300521
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