Global extreme precipitation characteristics: the perspective of climate and large river basins

• Published in: Climate dynamics Vol. 62; no. 2; pp. 1013 - 1030
• Main Authors: Zhao, Lili, Li, Lusheng, Li, Yanbin, Yang, Peiwen, Liu, Xiaomeng, Zhou, Zhaoqiang, Zhong, Huayu, Ding, Yibo
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01.02.2024; Springer Nature B.V
• Subjects: Annual precipitation; Arid climates; Basins; Climate; Climate and weather; Climate change; Climatology; Daily precipitation; Disasters; Earth and Environmental Science; Earth Sciences; Extreme weather; Flood control; Floods; Geophysics/Geodesy; Global climate; Global precipitation; Global warming; Hydrologic data; Natural disasters; Oceanography; Original Article; Polar climates; Precipitation; Precipitation data; Precipitation days; River basins; Rivers; Summer precipitation; Temperate climates; Warm climates; Waterlogging; Weather; Extreme precipitation; River basin; Global; Climate types
• ISSN: 0930-7575; 1432-0894
• DOI: 10.1007/s00382-023-06961-x

With global warming, extreme weather frequently and severely appears globally. Extreme precipitation is one of the extreme weather events that can cause many natural disasters, such as floods and waterlogging. In this study, Global Precipitation Climatology Project (GPCP) daily precipitation data were used to investigate extreme precipitation and its contribution to annual precipitation in different global climate regions and typical river basins. The climate types included equatorial climates (EC), arid climates (AC), warm temperate climates (WTC), snowy climates (SC) and polar climates (PC). R99p, Rx5day, CWD and R20 was selected as extreme precipitation indices in this study; extreme precipitation days were defined by CWD and R20. The results showed that EC and WTC had higher extreme precipitation level; SC and PC had lower extreme precipitation amounts and days than AC. R99p, Rx5day and CWD monitored higher extreme precipitation contribution degrees in AC; however, R20 monitored higher contribution degrees in EC and WTC. R99p, Rx5day and CWD showed higher extreme precipitation contribution degrees in North Africa, the Middle East, Australia and northwestern China; R20 showed higher contribution degrees in South America, the southeastern United States and South Asia. Based on historical observational data, Heilongjiang Basin (HB), Yellow River Basin (YERB), Yangtze River Basin (YARB), Ganges River Basin (GRB), Danube River Basin (DRB) and Mekong River Basin (MERB) had high-frequency extreme precipitation in summer. The research results are helpful for understanding the characteristics of extreme precipitation and provide a reference for flood control and disaster reduction in different climatic regions and main river basins.