Global coupled dynamics of tropical easterly waves and tropical cyclone genesis

被引:0
作者
Du, Xueqing [1 ]
Chu, Jung-Eun [1 ]
Jin, Fei-Fei [2 ]
Cheung, Hung Ming [3 ]
机构
[1] City Univ Hong Kong, Sch Energy & Environm, Hong Kong, Peoples R China
[2] Univ Hawaii Manoa, Sch Ocean & Earth Sci & Technol, Dept Atmospher Sci, Honolulu, HI USA
[3] Ewha Womans Univ, Severe Storm Res Ctr, Seoul, South Korea
来源
NPJ CLIMATE AND ATMOSPHERIC SCIENCE | 2025年 / 8卷 / 01期
基金
中国国家自然科学基金;
关键词
SYNOPTIC-SCALE WAVES; EQUATORIAL WAVES; SAHARAN DUST; ATLANTIC; NORTH; CYCLOGENESIS; INSTABILITY; CLIMATE; ORIGIN; JET;
D O I
10.1038/s41612-025-01014-y
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Tropical easterly waves (TEWs) are westward-moving waves often within trade winds but occur ubiquitously in the tropics and play a significant role in the genesis of tropical cyclones (TCs). They are well-known as primary precursors of TCs in the Atlantic, yet their global relationship with TCs has been less explored. This study, for the first time, presents the global distribution of TEW activity using a combined thermodynamic and dynamic framework based on 6-hourly Outgoing Longwave Radiation and curvature vorticity. We then demonstrate that TEWs play a dominant role in approximately 22-71% of global TC genesis, with their highest impacts in the North Atlantic (71%) and Western Pacific (54%). We further identify that TEWs, in their general coupling with TC genesis dynamics, act to intensify TC convection and vorticity in all TC main development regions, albeit the vorticity enhancement is relatively weaker in the North Atlantic. To understand the cross-basin differences in this general TEW-TC relationship, we further investigated background conditions for TC genesis in each basin and found an additional dry environment constraint in the Atlantic TC genesis, yet still delineating the critical role of TEWs in TC development.
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页数:9
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