Unprecedented Northern Hemisphere Tropical Cyclone Genesis in 2018 Shaped by Subtropical Warming in the North Pacific and the North Atlantic

被引:14
|
作者
Wang, Chao [1 ,2 ,3 ]
Wang, Bin [1 ,2 ,3 ]
Cao, Jian [1 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster Minist Educ, Joint Int Res Lab Climate & Environm Change, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing, Jiangsu, Peoples R China
[2] Univ Hawaii Manoa, Dept Atmospher Sci, Honolulu, HI 96822 USA
[3] Univ Hawaii Manoa, Int Pacific Res Ctr, Honolulu, HI 96822 USA
基金
中国国家自然科学基金;
关键词
Northern Hemisphere tropical cyclone season; North Pacific subtropical high; subtropical sea surface warming; tropical cyclone genesis; SEA-SURFACE TEMPERATURE; NINO-SOUTHERN-OSCILLATION; EL-NINO; HURRICANE FREQUENCY; MERIDIONAL MODE; VARIABILITY; INTENSITY; PREDICTABILITY; MONSOON; EASTERN;
D O I
10.1029/2019GL085406
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Northern Hemisphere tropical cyclone (TC) genesis (TCG) frequency in June-September of 2018 reached a record high since 1965. This unprecedented TCG was mainly driven by the North Pacific (NP) and the subtropical North Atlantic (NA). TCs in the western North Pacific (WNP) predominately took a northward-recurving track, resulting in the highest number of named storm days in the subtropical WNP on record. TCs in the eastern North Pacific propagated anomalously westward with three Category 4-5 hurricanes reaching the central North Pacific. The unprecedented TCG in the NP was caused by a persistent weakening of the NP subtropical high that was tightly coupled with the subtropical NP sea surface temperature (SST) warming. In the NA, enhanced TCG was mainly found in the subtropics owing to a favorable large-scale environment forced by subtropical SST warming. The result here has important implications for understanding variability in TC activity on the hemisphere-scale.
引用
收藏
页码:13327 / 13337
页数:11
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