Characteristics of the precipitation concentration and their relationship with the precipitation structure: A case study in the Huai River basin, China

被引:9
|
作者
Yin, Yixing [1 ]
Chen, Haishan [2 ]
Wang, Guojie [3 ]
Xu, Wucheng [4 ]
Wang, Shenmin [3 ]
Yu, Wenjun [1 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Sch Hydrol & Water Resources, Nanjing 210044, Jiangsu, Peoples R China
[2] Nanjing Univ Informat Sci & Technol, Minist Educ, Key Lab Meteorol Disaster, Nanjing 210044, Jiangsu, Peoples R China
[3] Nanjing Univ Informat Sci & Technol, Sch Geog Sci, Nanjing 210044, Peoples R China
[4] China West Normal Univ, Sch Land & Resources, Nanchong 637002, Peoples R China
基金
中国国家自然科学基金;
关键词
Precipitation concentration; Precipitation structure; Precipitation indices; Gini coefficient; Huai River basin; SPATIAL-DISTRIBUTION; SPATIOTEMPORAL VARIABILITY; RAINFALL CONCENTRATION; CONCENTRATION INDEX; TRENDS; EXTREMES; SPAIN; LINKS;
D O I
10.1016/j.atmosres.2021.105484
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Concentrated heavy precipitation has a great potential to cause severe flood disasters, especially in densely populated areas. However, the influencing factors of the spatio-temporal changes of precipitation concentration have not been well understood and the relationship between the characteristics of precipitation concentration and the structure of precipitation has rarely been investigated so far. This study explored the concentration characteristics of precipitation based on the Gini coefficient and further investigated the relationship of the precipitation concentration with the precipitation structure by means of a set of precipitation indices based on the daily precipitation data from 1960 to 2014 in the climatic transition zone of the Huai River basin (HRB), China. Results show that: (1) There is a non-significant upward trend for the Gini in the HRB. The mean of the Gini coefficient shows a spatial pattern of increase from the south to the north, and the standard deviation (SD) of the Gini shows a pattern of increase from the northeast to the southwest. (2) The composite mean of the Gini in the drought years is larger than that in the flood years for all the stations. And the composite SD of the Gini in the flood years is larger than that in the drought years for most of the stations. (3) The non-significant increase of the Gini in the HRB is mainly associated with AR (Annual rainfall), RD (Rainy days), the light and moderate rainfall (mainly PF20, PF40, PF50) and the wet-day and dry-day indices (PPWW, PWSAV, PPDD and PDSAV).
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页数:12
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