Potential benefits of limiting global warming for the mitigation of temperature extremes in China

被引:5
|
作者
Guo, Junhong [1 ]
Liang, Xi [2 ]
Wang, Xiuquan [3 ]
Fan, Yurui [4 ]
Liu, Lvliu [5 ]
机构
[1] North China Elect Power Univ, Coll Environm Sci & Engn, MOE, Key Lab Resource & Environm Syst Optimizat, Beijing 102206, Peoples R China
[2] UCL, Bartlett Sch Sustainable Construct, Sustainable Finance & Infrastruct Transit, London WC1E 6BT, England
[3] Univ Prince Edward Isl, Sch Climate Change & Adaptat, Charlottetown, PE C1A 4P3, Canada
[4] Brunel Univ, Dept Civil & Environm Engn, Uxbridge UB8 3PH, Middx, England
[5] China Meteorol Adm, Beijing Climate Ctr, Beijing, Peoples R China
关键词
CLIMATE; CMIP5; PRECIPITATION; INDEXES;
D O I
10.1038/s41612-023-00412-4
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In this study, we attempt to quantify the potential impacts of two global warming levels (i.e., 1.5 & DEG;C and 2.0 & DEG;C) on extreme temperature indices across China. The CMIP6 dataset is first evaluated against the CN05.1 observation for the historical period of 1995-2014. Then, future spatiotemporal patterns of changes in extreme temperature at two global warming levels under two shared socio-economic pathway scenarios (SSP245 and SSP585) are further analyzed. Overall, China will experience more frequent and intense high temperature events, such as summer days (SU), tropical nights (TR), warm days (TX90p) and nights (TN90p). On the other hand, under the SSP585, the number of icing days and frost days is projected to decrease at two global warming levels, with the maximal days of decrease (exceeding 20 days) seen in the west of China. Our results suggest that limiting global warming to 1.5 & DEG;C rather than 2.0 & DEG;C is beneficial to reduce extreme temperature risks. As temperature increases to 1.5 & DEG;C and then 2.0 & DEG;C above preindustrial levels, the most extreme temperature indices are expected to increase proportionately more during the final 0.5 & DEG; than during the first 1.5 & DEG; across most regions of China. For some warm indices, such as the warmest day (TXx), summer days (SU), and warm days (TX90p), the largest incremental changes (from 1.5 & DEG; to 2.0 & DEG;) tend to be found in the southwest. Under the SSP585, the incremental changes are similar to the change in the SSP245, but smaller magnitude and spatial extent.
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页数:10
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