Fronts and Cyclones Associated with Changes in the Total and Extreme Precipitation

被引:13
|
作者
Wu, Xinxin [1 ,3 ]
Tan, Xuezhi [1 ,2 ,3 ]
Liu, Bingjun [1 ,2 ,3 ]
Chen, Han [4 ]
Chen, Xiaohong [1 ,3 ]
机构
[1] Sun Yat Sen Univ, Ctr Water Resources & Environm, Guangzhou, Peoples R China
[2] Southern Marine Sci & Engn Guangdong Lab Zhuhai, Guangzhou, Peoples R China
[3] Sun Yat Sen Univ, Sch Civil Engn, Guangzhou, Peoples R China
[4] Hubei Inst Water Resources Survey & Design, Wuhan, Peoples R China
基金
中国国家自然科学基金;
关键词
Atmosphere; Asia; Climate change; Climate classification/regimes; Climate variability; Climatology; TROPICAL CYCLONES; EXTRATROPICAL CYCLONE; INCREASING TREND; ARID REGION; PART I; CHINA; RAINFALL; CLIMATE; TRACKING; LIFE;
D O I
10.1175/JCLI-D-21-0467.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Precipitation in China is controlled by a combination of multiple weather systems and is susceptible to their spatiotemporal variability under climate warming. Based on the daily precipitation dataset developed by the China Meteorological Administration and ERA5 6-hourly data from 1979 to 2018, we detected tropical cyclones, extratropical cyclones, and fronts affecting mainland China of an altitude less than 1500 m using objective methods and identified their individually associated precipitation. We quantified climatological characteristics of precipitation associated with these three meteorological causes and their proportion of precipitation totals, and evaluated their relative contribution to change in precipitation. Results show that precipitation associated with tropical cyclones (TCP), extratropical cyclones (ETCP), and fronts (FRTP) accounted for 3.0%, 21.2%, and 20.4% of the total precipitation in China, and constituted the largest percentage in August, June, and January, respectively. The total proportion of these three types of precipitation exceeded 50% in more than 55% of China's regions. The high-value regions of corresponding precipitation were directly related to the locations of frequent occurrences of these weather systems. TCP and FRTP increased over the past four decades, while ETCP decreased. The western part of Northeast China and the middle and upper reaches of the Yangtze River show precipitation decreases, 37.8% of which is contributed by ETCP decreases. Precipitation increased in most regions of China during the dry season, 34.1% of which is contributed by FRTP increases. Among them, Northeast (Northwest) China significantly increased it precipitation by 14.4% decade21 (21.8% decade21), 33.6%(51.3%) of which is contributed by FRTP increases.
引用
收藏
页码:4131 / 4146
页数:16
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