Impacts of climate change and anthropogenic stressors on runoff variations in major river basins in China since 1950

Xuelian Bai; Wenzhi Zhao

doi:10.1016/j.scitotenv.2023.165349

Impacts of climate change and anthropogenic stressors on runoff variations in major river basins in China since 1950

Sci Total Environ. 2023 Nov 10:898:165349. doi: 10.1016/j.scitotenv.2023.165349. Epub 2023 Jul 6.

Authors

Xuelian Bai¹, Wenzhi Zhao²

Affiliations

¹ Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; Linze Inland River Basin Research Station, Chinese Ecosystem Research Network, Lanzhou 730000, China; University of Chinese Academy of Sciences, Beijing 100029, China.
² Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; Linze Inland River Basin Research Station, Chinese Ecosystem Research Network, Lanzhou 730000, China. Electronic address: zhaowzh@lzb.ac.cn.

PMID: 37419363
DOI: 10.1016/j.scitotenv.2023.165349

Abstract

Runoff is one of the main components of hydrological cycle and an important index for water resources evaluation, understanding the runoff change and their causes is vital to water resource management. In the study, we analyzed the runoff change and the impacts of climate change and land use alteration on runoff variation based on natural runoff and previous studies in China. The results showed that there was a significant increasing trend in the annual runoff during 1961-2018 (p < 0.05), with change rate of 0.4 mm/a and abrupt point at 1999 across China, climate change dominated the runoff variation with a contribution of 54 %. In previous studies, the runoff of the major basins in China had a downward trend on the whole (-0.99 mm/a) except Continental River Basin (CRB) showed an increasing trend (0.25 mm/a), the abrupt points were mainly concentrated in 1991-2000, and human activity was the leading factor of runoff change with the contribution of 54 % across China. Human activity was the dominant factor of runoff change in Songhua and Liao River Basin (SLRB), Yellow River Basin (YRB), Hai River Basin (HRB) and Pearl River Basin (PRB), the contribution was >56 %, while climate change was the dominant factor of runoff change in Huai River Basin (HuRB), CRB, and Yangtze River Basin (YZRB). Overall, there was a significant correlation between runoff and precipitation, unused land, urban and grassland in China. We concluded that runoff change and the contribution of climate change and human activities varies greatly among different basins. The findings in this work can shed light on the quantitative understanding of runoff changes in national scale and offer a scientific basis for sustainable water management.

Keywords: Climate change; Land use change; River basins in China; Runoff.