globalchange  > 过去全球变化的重建
DOI: 10.1007/s00382-014-2134-4
Scopus记录号: 2-s2.0-84924021296
论文题名:
Modulation of Aleutian Low and Antarctic Oscillation co-variability by ENSO
作者: Li F.; Wang H.; Gao Y.
刊名: Climate Dynamics
ISSN: 9307575
出版年: 2015
卷: 44, 期:2017-05-06
起始页码: 1245
结束页码: 1256
语种: 英语
英文关键词: Aleutian Low ; Antarctic Oscillation ; El Niño–Southern Oscillation ; Interannual variability
英文摘要: We use both the National Centers for Environmental Prediction (NCEP)–National Center for Atmospheric Research (NCAR) reanalysis data (1979–2013) and the Community Atmospheric Model Version 3 to explore the modulation of El Niño–Southern Oscillation (ENSO) on the co-variability of the Aleutian Low (AL) and the Antarctic Oscillation (AAO). The empirical orthogonal function analysis on the NCEP–NCAR reanalysis data indicates that after the late-1990s the global sea level pressure (SLP) and 300-hPa geopotential height (Z300) in boreal January are characterized by the concurrence of the AL and the negative phase of the AAO (−AAO). Associated with this AL–AAO co-variation is a sea surface temperature anomaly that resembles the ENSO cycle. Further analyses reveal that the interdecadal change in ENSO signal (westward extension and more La Niña events) is responsible for the co-variability of AL and AAO after the late-1990s. Correspondingly, the El Niño-related anomalous heating and upward motion over the eastern–central equatorial Pacific can lead to the upper-tropospheric divergence in the western–central Pacific. This upper-tropospheric divergence plays an essential role in coupling the equatorial heat anomalies with the variation of the subtropical westerly jet of both hemispheres, and therefore results in the enhanced meridional circulation of the three cells. It thus implies that ENSO might act as a bridge linking AL and AAO after the late-1990s, causing their consistent co-variability. The numerical experiment also supports this hypothesis. © 2014, Springer-Verlag Berlin Heidelberg.
资助项目: NSFC, National Natural Science Foundation of China ; NSFC, National Natural Science Foundation of China
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/54220
Appears in Collections:过去全球变化的重建

Files in This Item:

There are no files associated with this item.


作者单位: Nansen-Zhu International Research Center, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China; Climate Change Research Center, Chinese Academy of Sciences, Beijing, China; University of Chinese Academy of Sciences, Beijing, China; Nansen Environmental and Remote Sensing Center and Bjerknes Centre for Climate Research, Bergen, Norway

Recommended Citation:
Li F.,Wang H.,Gao Y.. Modulation of Aleutian Low and Antarctic Oscillation co-variability by ENSO[J]. Climate Dynamics,2015-01-01,44(2017-05-06)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Li F.]'s Articles
[Wang H.]'s Articles
[Gao Y.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Li F.]'s Articles
[Wang H.]'s Articles
[Gao Y.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Li F.]‘s Articles
[Wang H.]‘s Articles
[Gao Y.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.