中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The different relationship of Pacific interior subtropical cells and two types of ENSO

文献类型:期刊论文

作者Feng, Junqiao1,2,3; Hu, Dunxin1,2,3; Jin, Fei-fei4; Jia, Fan1,2,3; Wang, Qingye1,2,3; Guan, Shoude1,2,3
刊名JOURNAL OF OCEANOGRAPHY
出版日期2018-10-01
卷号74期号:5页码:523-539
关键词Pacific Ocean Subtropical-tropical cells El Nino-Southern oscillation Eastern Pacific El Nino Central Pacific El Nino
ISSN号0916-8370
DOI10.1007/s10872-018-0478-9
通讯作者Feng, Junqiao(fengjunqiao@qdio.ac.cn)
英文摘要The Pacific interior subtropical-tropical cells (STCs) and their relation to the two types of El Nino-Southern Oscillation (ENSO) are investigated by using GODAS reanalysis ocean data for the period of 1980-2017. The results show that the interior STC transport into the equatorial region across 9 degrees S and 9 degrees N has a close relationship with the eastern Pacific (EP) ENSO, while it is much weaker with the central Pacific (CP) ENSO. It is suggested that the effect of interior STCs on the tropical Pacific climate is reflected in its relation with the western Pacific thermocline depth or SSHA. During the EP El Nino, the anomalous interior STCs at 9 degrees S and 9 degrees N converge to the equatorial region from the lag months of - 25 to - 8, leading to an accumulation of heat content in the equatorial Pacific; from the lag months of - 8 to 10, they diverge poleward, inducing a discharge of equatorial heat content. The peak poleward interior STC anomaly first appears at 9 degrees N at a zero-lag time, while that at 9 degrees S is observed 4-5months later. But there is also no appearance of a time lag between the interior STCs at 9 degrees N and 9 degrees S in recharging the period during the EP La Nina mature phase. However, during CP El Nino, only the conspicuous anomalous interior STC divergence appears during the mature and decay phases for the lag months of - 2 to 10, with being symmetric at 9 degrees N and 9 degrees S.
资助项目Natural Science Foundation of China (NSFC)[41476017] ; Natural Science Foundation of China (NSFC)[41330963] ; Natural Science Foundation of China (NSFC)[41506016] ; Natural Science Foundation of China (NSFC)[41576014] ; Natural Science Foundation of China (NSFC)[41506023] ; NSFC-Shandong Joint Fund for Marine Science Research Centers[U1406401] ; Fund for Innovative Research Groups of the NSFC[41421005]
WOS研究方向Oceanography
语种英语
WOS记录号WOS:000444003000007
出版者SPRINGER
源URL[http://ir.qdio.ac.cn/handle/337002/160288]  
专题海洋研究所_海洋环流与波动重点实验室
通讯作者Feng, Junqiao
作者单位1.Chinese Acad Sci, Inst Oceanol, Qingdao, Peoples R China
2.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Nanhai Rd 7, Qingdao 266071, Peoples R China
3.Qingdao Natl Lab Marine Sci & Technol, Lab Ocean & Climate Dynam, Qingdao, Peoples R China
4.Univ Hawaii Manoa, Dept Atmospher Sci, SOEST, Honolulu, HI 96822 USA
推荐引用方式
GB/T 7714
Feng, Junqiao,Hu, Dunxin,Jin, Fei-fei,et al. The different relationship of Pacific interior subtropical cells and two types of ENSO[J]. JOURNAL OF OCEANOGRAPHY,2018,74(5):523-539.
APA Feng, Junqiao,Hu, Dunxin,Jin, Fei-fei,Jia, Fan,Wang, Qingye,&Guan, Shoude.(2018).The different relationship of Pacific interior subtropical cells and two types of ENSO.JOURNAL OF OCEANOGRAPHY,74(5),523-539.
MLA Feng, Junqiao,et al."The different relationship of Pacific interior subtropical cells and two types of ENSO".JOURNAL OF OCEANOGRAPHY 74.5(2018):523-539.

入库方式: OAI收割

来源:海洋研究所

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