Future Projections of Multiple Tropical Cyclone Events in the Northern Hemisphere in the CMIP6-HighResMIP Models

被引:7
|
作者
Fu, Zheng-Hang [1 ]
Zhan, Ruifen [1 ,2 ,3 ]
Zhao, Jiuwei [4 ,5 ]
Yamada, Yohei [6 ]
Song, Kexin [1 ]
机构
[1] Fudan Univ, Inst Atmospher Sci, Dept Atmospher & Ocean Sci, Shanghai, Peoples R China
[2] Shanghai Qi Zhi Inst, Shanghai, Peoples R China
[3] Fudan Univ, Shanghai Key Lab Ocean Land Atmosphere Boundary Dy, Shanghai, Peoples R China
[4] Nanjing Univ Informat Sci & Technol NUIST, Sch Atmospher Sci, Nanjing, Peoples R China
[5] Nanjing Univ Informat Sci & Technol NUIST, Inst Climate & Applicat Res ICAR, Nanjing, Peoples R China
[6] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Tokyo, Japan
基金
中国国家自然科学基金;
关键词
multiple tropical cyclone events; future projections; Northern Hemisphere; CMIP6-HighResMIP; DGPI; EXPERIMENTAL-DESIGN; CLIMATE; RESOLUTION; INTENSIFICATION; SIMULATIONS; VARIABILITY; INTENSITY; FREQUENCY; PACIFIC; IMPACTS;
D O I
10.1029/2023GL103064
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
How future multiple tropical cyclone events (MTCEs) could change is crucial for effective risk management and ensuring human safety, however, it remains unclear. This study projects changes in MTCEs by 2050 in the major basins of the Northern Hemisphere using high-resolution climate models. Results show a significant increase in the frequency and duration of MTCEs over the North Atlantic (NA), a notable decrease over the western North Pacific (WNP), and little change over the eastern North Pacific (ENP). The increase in MTCEs over the NA is concentrated in August-September, while the decrease over the WNP occurs in most months. In contrast, the ENP exhibits large yet insignificant seasonal variation, suggesting considerable uncertainty in this basin. Further analysis shows that mid-level vertical motion dominates the MTCE changes over the WNP, while vertical wind shear contributes the most to the NA, which may be linked to future changes in tropical convection.
引用
收藏
页数:11
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