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DOI10.1175/JCLI-D-20-0087.1
Possible influence of tropical indian ocean sea surface temperature on the proportion of rapidly intensifying western north pacific tropical cyclones during the extended boreal summer
Gao J.; Zhao H.; Klotzbach P.J.; Wang C.; Raga G.B.; Chen S.
发表日期2020
ISSN0894-8755
起始页码9129
结束页码9143
卷号33期号:21
英文摘要This study examines the possible impact of tropical Indian Ocean (TIO) sea surface temperature anomalies (SSTAs) on the proportion of rapidly intensifying tropical cyclones (PRITC) over the western North Pacific (WNP) during the extended boreal summer (July-November). There is a robust interannual association (r = 0.46) between TIO SSTAs and WNP PRITC during 1979-2018. Composite analyses between years with warm and cold TIO SSTAs confirm a significant impact of TIO SSTA on WNP PRITC, with PRITC over the WNP basin being 50% during years with warm TIO SSTAs and 37% during years with cold TIO SSTAs. Tropical cyclone heat potential appears to be one of the most important factors in modulating the interannual change of PRITC over the WNP with a secondary role from midlevel moisture changes. Interannual changes in these large-scale factors respond to SSTA differences characterized by a tropics-wide warming, implying a possible global warming amplification on WNP PRITC. The possible footprint of global warming amplification of the TIO is deduced from 1) a significant correlation between TIO SSTAs and global mean SST (GMSST) and a significant linear increasing trend of GMSST and TIO SSTAs, and 2) an accompanying small difference of PRITC (∼8%) between years with detrended warm and cold TIO SSTAs compared to the difference of PRITC (∼13%) between years with nondetrended warm and cold TIO SSTAs. Global warming may contribute to increased TCHP, which is favorable for rapid intensification, but increased vertical wind shear is unfavorable for TC genesis, thus amplifying WNP PRITC. © 2020 American Meteorological Society.
英文关键词Atmospheric temperature; Global warming; Hurricanes; Storms; Submarine geophysics; Surface properties; Surface waters; Tropics; Composite analysis; Rapid intensification; Sea surface temperature (SST); Sea surface temperature anomalies; Tropical cyclone; Tropical Indian ocean; Vertical wind shear; Western North Pacific; Oceanography; annual variation; climate change; climate effect; climate variation; cyclogenesis; global warming; sea surface temperature; summer; temperature anomaly; tropical cyclone; vorticity; wind shear; Indian Ocean; Indian Ocean (Tropical); Pacific Ocean; Pacific Ocean (North)
语种英语
来源期刊Journal of Climate
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/171055
作者单位Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science and Technology, Nanjing, China; Key Laboratory of South China Sea Meteorological Disaster Prevention and Mitigation of Hainan, Haikoum, China; Key Laboratory of Meteorological Disaster, Ministry of Education, Joint International Research Laboratory of Climate and Environment Change, Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disaster, Pacific Typhoon Research Center, Earth System Modeling Center, Nanjing University of Information Science and Technology, Nanjing, China; Department of Atmospheric Science, Colorado State University, Fort Collins, CO, United States; Centro de Ciencias de la Atmósfera, Universidad Nacional Autónoma de Mexico, Mexico City, Mexico
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Gao J.,Zhao H.,Klotzbach P.J.,et al. Possible influence of tropical indian ocean sea surface temperature on the proportion of rapidly intensifying western north pacific tropical cyclones during the extended boreal summer[J],2020,33(21).
APA Gao J.,Zhao H.,Klotzbach P.J.,Wang C.,Raga G.B.,&Chen S..(2020).Possible influence of tropical indian ocean sea surface temperature on the proportion of rapidly intensifying western north pacific tropical cyclones during the extended boreal summer.Journal of Climate,33(21).
MLA Gao J.,et al."Possible influence of tropical indian ocean sea surface temperature on the proportion of rapidly intensifying western north pacific tropical cyclones during the extended boreal summer".Journal of Climate 33.21(2020).
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