Diurnal Variations on the Initiation Time and Intensification Rate of Rapidly Intensifying Tropical Cyclones

被引:2
|
作者
Zhang, Xinyan [1 ,2 ,3 ]
Xu, Weixin [1 ,2 ,3 ]
机构
[1] Sun Yat Sen Univ, Southern Marine Sci & Engn Guangdong Lab Zhuhai, Zhuhai, Peoples R China
[2] Sun Yat Sen Univ, Sch Atmospher Sci, Zhuhai, Peoples R China
[3] Guangdong Prov Key Lab Climate Change & Nat Disast, Guangzhou, Peoples R China
基金
中国国家自然科学基金;
关键词
tropical cyclone; rapid intensification; diurnal cycle; inner-core convection; intensity change; SEA-SURFACE TEMPERATURE; RELATIVE IMPORTANCE; RADIATION CYCLE; PRECIPITATION; RAINFALL; IMPACT; CHINA; CONVECTION; EVOLUTION; PULSES;
D O I
10.1029/2023GL103551
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This study investigates whether the initiation time and intensification rate (INTRATE) of intensifying tropical cyclones (TCs) vary diurnally and how they are related to deep convection. TC intensifying events are identified and classified into slowly intensifying (SI) and rapidly intensifying (RI) events. RI events last & SIM;42 hr on average, much longer than SI events. More importantly, the onset of the TC intensification, especially RI, markedly peaks at 00-06 local time. However, the INTRATEs of both RI and SI events show very weak diurnal variability. The INTRATE continues to increase after RI initiation and slightly peaks in the late afternoon (at 90% significance level). Inner-core convection of all intensifying events maximizes in the early morning, in phase with the peak initiation time. In short, our results suggest that the nocturnally enhanced inner-core convection may play a role in triggering TC intensification (e.g., RI), but not maximizing the INTRATE.
引用
收藏
页数:10
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