Increasing trends in rainfall erosivity in the Yellow River basin from 1971 to 2020

被引:0
|
作者
Wang, W. [1 ,2 ]
Yin, S. [2 ]
Gao, G. [3 ,4 ]
Papalexiou, S. M. [5 ]
Wang, Z. [6 ,7 ]
机构
[1] Beijing Normal Univ, Coll Educ Future, Zhuhai 519087, Peoples R China
[2] Beijing Normal Univ, Fac Geog Sci, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China
[3] China Meteorol Adm, Lab Climate Studies, Natl Climate Ctr, Beijing, Peoples R China
[4] Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing, Peoples R China
[5] Univ Saskatchewan, Dept Civil Geol & Environm Engn, Saskatoon, SK, Canada
[6] Xiamen Univ, MOE Key Lab Econometr, Wang Yanan Inst Studies Econ, Xiamen 361005, Fujian, Peoples R China
[7] Xiamen Univ, Sch Econ, Xiamen 361005, Fujian, Peoples R China
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
Yellow River basin; Rainfall erosivity; Extreme precipitation; Sediment reduction; Climate change; LATE-SUMMER PRECIPITATION; EXTREME RAINFALL; LOESS PLATEAU; SPATIOTEMPORAL VARIATION; TEMPORAL VARIABILITY; EASTERN CHINA; INTENSITY; DURATION; EVENTS; FREQUENCY;
D O I
10.1016/j.jhydrol.2022.127851
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Hourly precipitation data from 1971 to 2020, collected from 98 stations distributed across the Yellow River basin, were analyzed to detect changes in characteristics on rainfall and rainfall erosivity for all storms and storms with extreme erosivity (greater than 90th percentile). Results showed that over the past 50 years, rainfall erosivity at both event and seasonal scales over the whole basin increased significantly (p < 0.05) with rates of 5.46% and 6.86% decade-1, respectively, compared to the 1981-2010 average values. Approximate 80% of 98 stations showed increasing trends and 20% of stations had statistically significant trends (p < 0.1). The increase of rainfall erosivity resulted from the significant increasing trends of average storm precipitation (p < 0.1), duration (p < 0.1), rainfall energy (p < 0.05) and maximum 1-h intensity (p < 0.05). In addition, the total extreme erosivity showed significant upward trends at a relative rate of 6.05% decade(-1) (p < 0.05). Extreme erosivity storms occurred more frequently and with higher rainfall energy during the study period (p < 0.05). Trends for seasonal total and extreme erosivity were also estimated based on daily rainfall data, and the changing magnitudes were similar to those based on hourly rainfall data, which suggested daily rainfall can be applied to detect interannual and long-term variations of rainfall erosivity in the absence of rainfall data with higher resolution. It was suggested that soil and water conservation strategies and vegetation projects conducted within the Yellow River basin should be continued and enhanced in the future.
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页数:13
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