Response of runoff to climate change in the area of runoff yield in upstream Shiyang River Basin, Northwest China: A case study of the Xiying River

The objective of this study was to analyze the response of runoff in the area of runoff yield of the upstream Shiyang River basin to climate change and to promote sustainable development of regional water resources and ecological environment. As the biggest tributary of the Shiyang River, Xiying Riv...

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Main Authors: Shu-hong Song, Zhen-long Nie, Xin-xin Geng, Xue Shen, Zhe Wang, Pu-cheng Zhu
Format: Article
Language:English
Published: Groundwater Science and Engineering Limited 2023-03-01
Series:Journal of Groundwater Science and Engineering
Subjects:
Online Access:https://www.sciopen.com/article/10.26599/JGSE.2023.9280009
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author Shu-hong Song
Zhen-long Nie
Xin-xin Geng
Xue Shen
Zhe Wang
Pu-cheng Zhu
author_facet Shu-hong Song
Zhen-long Nie
Xin-xin Geng
Xue Shen
Zhe Wang
Pu-cheng Zhu
author_sort Shu-hong Song
collection DOAJ
description The objective of this study was to analyze the response of runoff in the area of runoff yield of the upstream Shiyang River basin to climate change and to promote sustainable development of regional water resources and ecological environment. As the biggest tributary of the Shiyang River, Xiying River is the only hydrological station (Jiutiaoling) that has provincial natural river and can achieve long time series monitoring data in the basin. The data obtained from this station is representative of natural conditions because it has little human activites. This study built a regression model through identifying the characteristics of runoff and climate change by using Mann-Kendall nonparametric statistical test, cumulative anomaly, and correlation analysis. The results show that the average annual runoff is 320.6 million m3/a with the coefficient of variation of 0.18 and shows slightly decrease during 1956–2020. It has a significant positive correlation the average annual precipitation (P<0.01). Runoff is sensitive to climate change, and the climate has becoming warm and wet and annual runoff has entering wet period from 2003. Compared to the earlier period (1955–2000), the increases of average annual temperature, precipitation and runoff in recent two decades were 15%, 9.3%, and 7.8%, respectively. Runoff in the Shiyang River is affected by temperature and precipitation among climate factors, and the simulation results of the runoff-climate response model (R = 0.0052P − 0.1589T + 2.373) indicate that higher temperature leads to a weakening of the ecological regulation of surface runoff in the flow-producing area.
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spelling doaj.art-534d29b3ad5f4cc9ab8306cbdaf173652023-04-24T05:59:48ZengGroundwater Science and Engineering LimitedJournal of Groundwater Science and Engineering2305-70682023-03-01111899610.26599/JGSE.2023.9280009Response of runoff to climate change in the area of runoff yield in upstream Shiyang River Basin, Northwest China: A case study of the Xiying RiverShu-hong Song0Zhen-long Nie1Xin-xin Geng2Xue Shen3Zhe Wang4Pu-cheng Zhu5Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, ChinaInstitute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, ChinaInstitute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, ChinaChina University of Geosciences , Beijing 10083, ChinaInstitute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, ChinaInstitute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, ChinaThe objective of this study was to analyze the response of runoff in the area of runoff yield of the upstream Shiyang River basin to climate change and to promote sustainable development of regional water resources and ecological environment. As the biggest tributary of the Shiyang River, Xiying River is the only hydrological station (Jiutiaoling) that has provincial natural river and can achieve long time series monitoring data in the basin. The data obtained from this station is representative of natural conditions because it has little human activites. This study built a regression model through identifying the characteristics of runoff and climate change by using Mann-Kendall nonparametric statistical test, cumulative anomaly, and correlation analysis. The results show that the average annual runoff is 320.6 million m3/a with the coefficient of variation of 0.18 and shows slightly decrease during 1956–2020. It has a significant positive correlation the average annual precipitation (P<0.01). Runoff is sensitive to climate change, and the climate has becoming warm and wet and annual runoff has entering wet period from 2003. Compared to the earlier period (1955–2000), the increases of average annual temperature, precipitation and runoff in recent two decades were 15%, 9.3%, and 7.8%, respectively. Runoff in the Shiyang River is affected by temperature and precipitation among climate factors, and the simulation results of the runoff-climate response model (R = 0.0052P − 0.1589T + 2.373) indicate that higher temperature leads to a weakening of the ecological regulation of surface runoff in the flow-producing area.https://www.sciopen.com/article/10.26599/JGSE.2023.9280009runoffheating and wettingmann-kendall testregression modelecological function
spellingShingle Shu-hong Song
Zhen-long Nie
Xin-xin Geng
Xue Shen
Zhe Wang
Pu-cheng Zhu
Response of runoff to climate change in the area of runoff yield in upstream Shiyang River Basin, Northwest China: A case study of the Xiying River
Journal of Groundwater Science and Engineering
runoff
heating and wetting
mann-kendall test
regression model
ecological function
title Response of runoff to climate change in the area of runoff yield in upstream Shiyang River Basin, Northwest China: A case study of the Xiying River
title_full Response of runoff to climate change in the area of runoff yield in upstream Shiyang River Basin, Northwest China: A case study of the Xiying River
title_fullStr Response of runoff to climate change in the area of runoff yield in upstream Shiyang River Basin, Northwest China: A case study of the Xiying River
title_full_unstemmed Response of runoff to climate change in the area of runoff yield in upstream Shiyang River Basin, Northwest China: A case study of the Xiying River
title_short Response of runoff to climate change in the area of runoff yield in upstream Shiyang River Basin, Northwest China: A case study of the Xiying River
title_sort response of runoff to climate change in the area of runoff yield in upstream shiyang river basin northwest china a case study of the xiying river
topic runoff
heating and wetting
mann-kendall test
regression model
ecological function
url https://www.sciopen.com/article/10.26599/JGSE.2023.9280009
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