Impacts of Climate Change and Human Activities on the Surface Runoff in the Wuhua River Basin

The impacts of climate change and human activities on the surface runoff in the Wuhua River Basin (hereinafter referred to as the river basin) are explored using the Mann–Kendall trend test, wavelet analysis, and double-mass curve. In this study, all the temperature and precipitation data...

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Main Authors: Zhengdong Zhang, Luwen Wan, Caiwen Dong, Yichun Xie, Chuanxun Yang, Ji Yang, Yong Li
Format: Article
Language:English
Published: MDPI AG 2018-09-01
Series:Sustainability
Subjects:
Online Access:http://www.mdpi.com/2071-1050/10/10/3405
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spelling doaj-331b455f060d41f5a5aa729a36f825862020-11-24T21:51:18ZengMDPI AGSustainability2071-10502018-09-011010340510.3390/su10103405su10103405Impacts of Climate Change and Human Activities on the Surface Runoff in the Wuhua River BasinZhengdong Zhang0Luwen Wan1Caiwen Dong2Yichun Xie3Chuanxun Yang4Ji Yang5Yong Li6School of Geography Sciences, South China Normal University, Guangzhou 510631, ChinaDepartment of Earth and Environmental Sciences, Michigan State University, East Lansing, MI 48823, USAThe Bureau of Land and Resources Huangshi, Huangshi 435000, ChinaInstitute for Geospatial Research and Education, Eastern Michigan University, Ypsilanti, MI 48197, USAGuangzhou Institute of Geography, Guangzhou 510070, ChinaGuangzhou Institute of Geography, Guangzhou 510070, ChinaGuangzhou Institute of Geography, Guangzhou 510070, ChinaThe impacts of climate change and human activities on the surface runoff in the Wuhua River Basin (hereinafter referred to as the river basin) are explored using the Mann–Kendall trend test, wavelet analysis, and double-mass curve. In this study, all the temperature and precipitation data from two meteorological stations, namely, Wuhua and Longchuan, the measured monthly runoff data in Hezikou Hydrological Station from 1961 to 2013, and the land-cover type data in 1990 and 2013 are used. This study yields valuable results. First, over the past 53 years, the temperature in the river basin rose substantially, without obvious changes in the average annual precipitation. From 1981 to 2013, the annual runoff fluctuated and declined, and this result is essentially in agreement with the time-series characteristics of precipitation. Second, both temperature and precipitation had evidently regular changes on the 28a scale, and the annual runoff changed on the 19a scale. Third, forestland was the predominant land use type in the Wuhua river basin, followed by cultivated land. Major transitions mainly occurred in both land-use types, which were partially transformed into grassland and construction land. From 1990 to 2013, cultivated land was the most active land-use type in the transitions, and construction land was the most stable type. Finally, human activities had always been a decisive factor on the runoff reduction in the river basin, accounting for 85.8%. The runoff in the river basin suffered most heavily from human activities in the 1980s and 1990s, but thereafter, the impact of these activities diminished to a certain extent. This may be because of the implementation of water loss and soil erosion control policies.http://www.mdpi.com/2071-1050/10/10/3405runoffland-use changeclimate changehuman activitiesWuhua River
collection DOAJ
language English
format Article
sources DOAJ
author Zhengdong Zhang
Luwen Wan
Caiwen Dong
Yichun Xie
Chuanxun Yang
Ji Yang
Yong Li
spellingShingle Zhengdong Zhang
Luwen Wan
Caiwen Dong
Yichun Xie
Chuanxun Yang
Ji Yang
Yong Li
Impacts of Climate Change and Human Activities on the Surface Runoff in the Wuhua River Basin
Sustainability
runoff
land-use change
climate change
human activities
Wuhua River
author_facet Zhengdong Zhang
Luwen Wan
Caiwen Dong
Yichun Xie
Chuanxun Yang
Ji Yang
Yong Li
author_sort Zhengdong Zhang
title Impacts of Climate Change and Human Activities on the Surface Runoff in the Wuhua River Basin
title_short Impacts of Climate Change and Human Activities on the Surface Runoff in the Wuhua River Basin
title_full Impacts of Climate Change and Human Activities on the Surface Runoff in the Wuhua River Basin
title_fullStr Impacts of Climate Change and Human Activities on the Surface Runoff in the Wuhua River Basin
title_full_unstemmed Impacts of Climate Change and Human Activities on the Surface Runoff in the Wuhua River Basin
title_sort impacts of climate change and human activities on the surface runoff in the wuhua river basin
publisher MDPI AG
series Sustainability
issn 2071-1050
publishDate 2018-09-01
description The impacts of climate change and human activities on the surface runoff in the Wuhua River Basin (hereinafter referred to as the river basin) are explored using the Mann–Kendall trend test, wavelet analysis, and double-mass curve. In this study, all the temperature and precipitation data from two meteorological stations, namely, Wuhua and Longchuan, the measured monthly runoff data in Hezikou Hydrological Station from 1961 to 2013, and the land-cover type data in 1990 and 2013 are used. This study yields valuable results. First, over the past 53 years, the temperature in the river basin rose substantially, without obvious changes in the average annual precipitation. From 1981 to 2013, the annual runoff fluctuated and declined, and this result is essentially in agreement with the time-series characteristics of precipitation. Second, both temperature and precipitation had evidently regular changes on the 28a scale, and the annual runoff changed on the 19a scale. Third, forestland was the predominant land use type in the Wuhua river basin, followed by cultivated land. Major transitions mainly occurred in both land-use types, which were partially transformed into grassland and construction land. From 1990 to 2013, cultivated land was the most active land-use type in the transitions, and construction land was the most stable type. Finally, human activities had always been a decisive factor on the runoff reduction in the river basin, accounting for 85.8%. The runoff in the river basin suffered most heavily from human activities in the 1980s and 1990s, but thereafter, the impact of these activities diminished to a certain extent. This may be because of the implementation of water loss and soil erosion control policies.
topic runoff
land-use change
climate change
human activities
Wuhua River
url http://www.mdpi.com/2071-1050/10/10/3405
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