Diurnal Variations in Different Precipitation Duration Events over the Yangtze River Delta Urban Agglomeration

被引:6
|
作者
Yao, Rui [1 ,2 ,3 ]
Zhang, Shuliang [1 ,2 ,3 ]
Sun, Peng [4 ,5 ]
Bian, Yaojin [4 ]
Yang, Qiqi [1 ,2 ,3 ]
Guan, Zongkui [1 ,2 ,3 ]
Zhang, Yaru [1 ,2 ,3 ]
机构
[1] Nanjing Normal Univ, Sch Geog, Nanjing 210023, Peoples R China
[2] Nanjing Normal Univ, Key Lab VGE, Minist Educ, Nanjing 210023, Peoples R China
[3] Nanjing Normal Univ, Jiangsu Ctr Collaborat Innovat Geog Informat Reso, Nanjing 210023, Peoples R China
[4] Anhui Normal Univ, Sch Geog & Tourism, Wuhu 241002, Peoples R China
[5] China Univ Geosci, Natl Engn Res Ctr Geog Informat Syst, Wuhan 430074, Peoples R China
基金
中国国家自然科学基金;
关键词
diurnal variation; precipitation duration; urbanization; Yangtze River Delta Urban Agglomeration; EXTREME HOURLY PRECIPITATION; LATE-SUMMER PRECIPITATION; EASTERN CHINA; URBANIZATION; FREQUENCY; RAINFALL; IMPACT; CYCLE; TEMPERATURE; SEASONALITY;
D O I
10.3390/rs14205244
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Studying the characteristics of precipitation diurnal variation is beneficial for understanding precipitation formation and underlying mechanisms. In this study, using hourly rain gauge data from 108 stations in the Yangtze River Delta Urban Agglomeration (YRDUA) from 1980-2021, the diurnal variations of the precipitation amount (PA), precipitation frequency (PF), precipitation duration (PD), and precipitation intensity (PI) were analyzed. The effects of elevation, distance of the station from the east coastline, and urbanization on the characteristics of different precipitation duration events were determined. The results indicated that (1) the spatial distributions of PA, PD, and PF were similar in short-duration (SD), long-duration (LD), and ultra-long-duration (ULD), with high values in the south and low values in the north. Most of PA, PD, and PF showed an increasing trend after breakpoint in LD and ULD, but precipitation characteristics in SD showed a decreasing trend before and after breakpoint; (2) the diurnal cycles of PA presented two comparable peaks in the late afternoon and early morning, which occurred SD and ULD precipitation events, respectively. A single peak in the late afternoon (15:00 local solar time [LST]) occurred during the diurnal cycle of PI. The start and peak times occurred mainly in the afternoon for SD and LD. In contrast, the peak time of ULD mainly occurred in the early morning, accounting for 63% of the stations. The start and peak times of LD and ULD occurred in the early morning mainly along the Yangtze River; (3) from the plains to the mountains, the diurnal peaks of PA and PI had gradual variations from noon to afternoon. In addition, dominant diurnal peak values of PA and PI, which are affected by the distance from the east coast, were observed in the early morning in ULD. The effect of urbanization on the difference between urban and rural areas changed from negative to positive after 2000. In addition, urbanization had a significant impact on SD. After 2000, the increase of PA in urban areas was mainly due to the obvious increase of PD and PF in SD, while the increasing trend of LD and ULD in urban areas was smaller than that in rural areas.
引用
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页数:18
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