Changes of Southern Hemisphere westerlies in the future warming climate

被引:42
|
作者
Deng, Kaiqiang [1 ,2 ,4 ]
Azorin-Molina, Cesar [2 ,3 ]
Yang, Song [1 ,4 ]
Hu, Chundi [1 ,4 ]
Zhang, Gangfeng [5 ,6 ,7 ]
Minola, Lorenzo [2 ]
Chen, Deliang [2 ]
机构
[1] Sun Yat Sen Univ, Sch Atmospher Sci, Southern Marine Sci & Engn Guangdong Lab Zhuhai, Zhuhai 519082, Guangdong, Peoples R China
[2] Univ Gothenburg, Dept Earth Sci, Reg Climate Grp, S-40530 Gothenburg, Sweden
[3] Consejo Super Invest Cient CIDE CSIC UV GVA, Ctr Invest Desertificac, Valencia, Spain
[4] Sun Yat sen Univ, Guangdong Prov Key Lab Climate Change & Nat Disas, Zhuhai 519082, Guangdong, Peoples R China
[5] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China
[6] Beijing Normal Univ, Acad Disaster Reduct & Emergency Management, Minist Emergency Management, Beijing 100875, Peoples R China
[7] Beijing Normal Univ, Minist Educ, Beijing 100875, Peoples R China
基金
瑞典研究理事会; 中国国家自然科学基金;
关键词
Southern Hemisphere westerlies; Human activities; Future projections; CMIP6; ANNULAR MODE; HADLEY CIRCULATION; TRENDS; OCEAN; VENTILATION; CMIP6; WINDS;
D O I
10.1016/j.atmosres.2022.106040
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Southern Hemisphere westerlies (SHWs) play a key role in regulating global climate and ocean circulation, but their future changes under low to high greenhouse gas forcings remain unclear. This study investigates the long-term trends in strength and position of the SHWs and their linkage with human activities, based on the ERA5 reanalysis and model simulations from the Coupled Model Intercomparison Project phase 6 (CMIP6). The results show that the SHWs have intensified and shifted poleward in the recent decades, and are projected to experience divergent trends in strength and position during the 21st century under different Shared Socioeco-nomic Pathway (SSP) scenarios. Forced by SSP245, 370, and 585, which represent the middle to high greenhouse gas forcings, the SHWs will continue to strengthen and move southward in 2015-2099, with the largest trends induced by SSP585. Nevertheless, forced by SSP126, which implies a low greenhouse gas forcing in the future, the ongoing trends in strength and position of the SHWs will be interrupted and even reversed. Further inves-tigation reveals that the anthropogenic forcing could have affected and will likely influence the SHWs by modulating meridional atmospheric circulation in the Southern Hemisphere. In particular, the Southern Annular Mode and the tropical Pacific convection play crucial roles in the changes of SHWs. This study links human activities to the changes in SHWs, providing important implications for climate change and its mitigation.
引用
收藏
页数:12
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