Future Changes of Extreme Precipitation and Related Atmospheric Conditions in East Asia under Global Warming Projected in Large Ensemble Climate Prediction Data

被引:1
作者
He, Sicheng [1 ,2 ]
Takemi, Tetsuya [1 ]
机构
[1] Kyoto Univ, Disaster Prevent Res Inst, Uji, Kyoto, Japan
[2] Kyoto Univ, Grad Sch Sci, Kyoto, Japan
基金
日本学术振兴会;
关键词
Extreme events; Precipitation; Climate change; Climate models; Model evaluation/performance; PART I; MODEL; SIMULATIONS; TEMPERATURE; VARIABILITY; STABILITY; INCREASES; FREQUENCY; MOISTURE; IMPACTS;
D O I
10.1175/JCLI-D-22-0924.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Extreme precipitation is expected to pose a more severe threat to human society in the future. This work assessed the historical performance and future changes in extreme precipitation and related atmospheric conditions in a large ensemble climate prediction dataset, the database for Policy Decision-making for Future climate change (d4PDF), over East Asia. Compared with the Tropical Rainfall Measuring Mission (TRMM) and fi fth major global reanalysis produced by ECMWF (ERA5) datasets, the historical climate in d4PDF represents favorably the precipitation characteristics and the atmospheric conditions, although some differences are notable in the moisture, vertical motion, and cloud water fi elds. The future climate projection indicates that both the frequency and intensity of heavy precipitation events over East Asia increase compared with those in the present climate. However, when comparing the atmospheric conditions in the historical and future climates for the same precipitation intensity range, the future climate indicates smaller relative humidity, weaker ascent, less cloud water content, and smaller temperature lapse rate, which negatively affect generating extreme precipitation events. The comparison of the precipitation intensity at the same amount of precipitable water between the historical and future climates indicates that extreme precipitation is weaker in the future because of the more stabilized troposphere in the future. The general increase in extreme precipitation under future climate is primarily due to the enhanced increase in precipitable water in the higher temperature ranges, which counteracts the negative conditions of the stabilized troposphere.
引用
收藏
页码:5171 / 5186
页数:16
相关论文
共 68 条
[1]  
Accadia C, 2003, WEATHER FORECAST, V18, P918, DOI 10.1175/1520-0434(2003)018<0918:SOPFSS>2.0.CO
[2]  
2
[3]   Constraints on future changes in climate and the hydrologic cycle [J].
Allen, MR ;
Ingram, WJ .
NATURE, 2002, 419 (6903) :224-+
[4]   Annual and seasonal mapping of peak intensity, magnitude and duration of extreme precipitation events across a climatic gradient, northeast Spain [J].
Begueria, Santiago ;
Vicente-Serrano, Sergio M. ;
Lopez-Moreno, Juan I. ;
Garcia-Ruiz, Jose M. .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2009, 29 (12) :1759-1779
[5]   SEA ICE THICKNESS DISTRIBUTION IN THE ARCTIC-OCEAN [J].
BOURKE, RH ;
GARRETT, RP .
COLD REGIONS SCIENCE AND TECHNOLOGY, 1987, 13 (03) :259-280
[6]  
C3s, 2018, ECMWR
[7]   Distinct effects of global mean warming and regional sea surface warming pattern on projected uncertainty in the South Asian summer monsoon [J].
Chen, Xiaolong ;
Zhou, Tianjun .
GEOPHYSICAL RESEARCH LETTERS, 2015, 42 (21) :9433-9439
[8]   Global Land Monsoon Precipitation Changes in CMIP6 Projections [J].
Chen, Ziming ;
Zhou, Tianjun ;
Zhang, Lixia ;
Chen, Xiaolong ;
Zhang, Wenxia ;
Jiang, Jie .
GEOPHYSICAL RESEARCH LETTERS, 2020, 47 (14)
[9]   Mechanisms for Global Warming Impacts on Precipitation Frequency and Intensity [J].
Chou, Chia ;
Chen, Chao-An ;
Tan, Pei-Hua ;
Chen, Kuan Ting .
JOURNAL OF CLIMATE, 2012, 25 (09) :3291-3306
[10]   Evaluating the "Rich-Get-Richer'' Mechanism in Tropical Precipitation Change under Global Warming [J].
Chou, Chia ;
Neelin, J. David ;
Chen, Chao-An ;
Tu, Jien-Yi .
JOURNAL OF CLIMATE, 2009, 22 (08) :1982-2005