The Spatiotemporal Variations of Runoff in the Yangtze River Basin under Climate Change

A better understanding of the runoff variations contributes to a better utilization of water resources and water conservancy planning. In this paper, we analyzed the runoff changes in the Yangtze River Basin (YRB) including the spatiotemporal characteristics of intra-annual variation, the trend, the...

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Main Authors: Ziwei Xiao, Peng Shi, Peng Jiang, Jianwei Hu, Simin Qu, Xingyu Chen, Yingbing Chen, Yunqiu Dai, Jianjin Wang
Format: Article
Language:English
Published: Wiley 2018-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2018/5903451
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author Ziwei Xiao
Peng Shi
Peng Jiang
Jianwei Hu
Simin Qu
Xingyu Chen
Yingbing Chen
Yunqiu Dai
Jianjin Wang
author_facet Ziwei Xiao
Peng Shi
Peng Jiang
Jianwei Hu
Simin Qu
Xingyu Chen
Yingbing Chen
Yunqiu Dai
Jianjin Wang
author_sort Ziwei Xiao
collection DOAJ
description A better understanding of the runoff variations contributes to a better utilization of water resources and water conservancy planning. In this paper, we analyzed the runoff changes in the Yangtze River Basin (YRB) including the spatiotemporal characteristics of intra-annual variation, the trend, the mutation point, and the period of annual runoff using various statistical methods. We also investigated how changes in the precipitation and temperature could impact on runoff. We found that the intra-annual runoff shows a decreasing trend from 1954 to 2008 and from upper stream to lower stream. On the annual runoff sequence, the upstream runoff has a high consistency and shows an increasing diversity from upper stream to lower stream. The mutation points of the annual runoff in the YRB are years 1961 and 2004. Annual runoff presents multitime scales for dry and abundance changes. Hurst values show that the runoffs at the main control stations all have Hurst phenomenon (the persistence of annual runoff). The sensitivity analyses of runoff variation to precipitation and temperature were also conducted. Our results show that the response of runoff to precipitation is more sensitive than that to temperature. The response of runoff to temperature is only one-third of the response to precipitation. A decrease in temperature may offset the impact of decreasing rainfall on runoff, while an increase in both rainfall and temperature leads to strongest runoff variations in the YRB.
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spelling doaj-art-38b5796504094bf4bbe8cca9068cf3fd2025-02-03T05:54:17ZengWileyAdvances in Meteorology1687-93091687-93172018-01-01201810.1155/2018/59034515903451The Spatiotemporal Variations of Runoff in the Yangtze River Basin under Climate ChangeZiwei Xiao0Peng Shi1Peng Jiang2Jianwei Hu3Simin Qu4Xingyu Chen5Yingbing Chen6Yunqiu Dai7Jianjin Wang8College of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaState Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, ChinaBureau of Hydrology, MWR, Beijing 100053, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaA better understanding of the runoff variations contributes to a better utilization of water resources and water conservancy planning. In this paper, we analyzed the runoff changes in the Yangtze River Basin (YRB) including the spatiotemporal characteristics of intra-annual variation, the trend, the mutation point, and the period of annual runoff using various statistical methods. We also investigated how changes in the precipitation and temperature could impact on runoff. We found that the intra-annual runoff shows a decreasing trend from 1954 to 2008 and from upper stream to lower stream. On the annual runoff sequence, the upstream runoff has a high consistency and shows an increasing diversity from upper stream to lower stream. The mutation points of the annual runoff in the YRB are years 1961 and 2004. Annual runoff presents multitime scales for dry and abundance changes. Hurst values show that the runoffs at the main control stations all have Hurst phenomenon (the persistence of annual runoff). The sensitivity analyses of runoff variation to precipitation and temperature were also conducted. Our results show that the response of runoff to precipitation is more sensitive than that to temperature. The response of runoff to temperature is only one-third of the response to precipitation. A decrease in temperature may offset the impact of decreasing rainfall on runoff, while an increase in both rainfall and temperature leads to strongest runoff variations in the YRB.http://dx.doi.org/10.1155/2018/5903451
spellingShingle Ziwei Xiao
Peng Shi
Peng Jiang
Jianwei Hu
Simin Qu
Xingyu Chen
Yingbing Chen
Yunqiu Dai
Jianjin Wang
The Spatiotemporal Variations of Runoff in the Yangtze River Basin under Climate Change
Advances in Meteorology
title The Spatiotemporal Variations of Runoff in the Yangtze River Basin under Climate Change
title_full The Spatiotemporal Variations of Runoff in the Yangtze River Basin under Climate Change
title_fullStr The Spatiotemporal Variations of Runoff in the Yangtze River Basin under Climate Change
title_full_unstemmed The Spatiotemporal Variations of Runoff in the Yangtze River Basin under Climate Change
title_short The Spatiotemporal Variations of Runoff in the Yangtze River Basin under Climate Change
title_sort spatiotemporal variations of runoff in the yangtze river basin under climate change
url http://dx.doi.org/10.1155/2018/5903451
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