IOCAS-IR  > 海洋环流与波动重点实验室
Ural Blocking as an Amplifier of the Arctic Sea Ice Decline in Winter
Gong, Tingting1; Luo, Dehai2
2017-04-01
Source PublicationJOURNAL OF CLIMATE
Volume30Issue:7Pages:2639-2654
SubtypeArticle
AbstractIn this paper, the lead-lag relationship between the Arctic sea ice variability over the Barents-Kara Sea (BKS) and Ural blocking (UB) in winter (DJF) ranging from 1979/80 to 2011/12 is examined. It is found that in a regressed DJF-mean field an increased UB frequency (days) corresponds to an enhanced sea ice decline over the BKS, while the high sea surface temperature over the BKS is accompanied by a significant Arctic sea ice reduction. Lagged daily regression and correlation reveal that the growth and maintenance of the UB that is related to the positive North Atlantic Oscillation (NAO(+)) through the negative east Atlantic/west Russia (EA/WR-) wave train is accompanied by an intensified negative BKS sea ice anomaly, and the BKS sea ice reduction lags the UB pattern by about four days. Because the intensified UB pattern occurs together with enhanced downward infrared radiation (IR) associated with the intensified moisture flux convergence and total column water over the BKS, the UB pattern contributes significantly to the BKS sea ice decrease on a time scale of weeks through intensified positive surface air temperature (SAT) anomalies resulting from enhanced downward IR. It is also found that the BKS sea ice decline can persistently maintain even when the UB has disappeared, thus indicating that the UB pattern is an important amplifier of the BKS sea ice reduction. Moreover, it is demonstrated that the EA/WR wave train formed by the combined NAO(+) and UB patterns is closely related to the amplified warming over the BKS through the strengthening (weakening) of mid-to-high-latitude westerly wind in the North Atlantic (Eurasia).
DOI10.1175/JCLI-D-16-0548.1
Indexed BySCI
Language英语
WOS IDWOS:000399678400020
Citation statistics
Document Type期刊论文
Version出版稿
Identifierhttp://ir.qdio.ac.cn/handle/337002/137064
Collection海洋环流与波动重点实验室
Affiliation1.Chinese Acad Sci, Inst Oceanog, Qingdao, Peoples R China
2.Chinese Acad Sci, CAS Key Lab Reg Climate Environm Temperate East A, Inst Atmospher Phys, Beijing, Peoples R China
First Author AffilicationInstitute of Oceanology, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Gong, Tingting,Luo, Dehai. Ural Blocking as an Amplifier of the Arctic Sea Ice Decline in Winter[J]. JOURNAL OF CLIMATE,2017,30(7):2639-2654.
APA Gong, Tingting,&Luo, Dehai.(2017).Ural Blocking as an Amplifier of the Arctic Sea Ice Decline in Winter.JOURNAL OF CLIMATE,30(7),2639-2654.
MLA Gong, Tingting,et al."Ural Blocking as an Amplifier of the Arctic Sea Ice Decline in Winter".JOURNAL OF CLIMATE 30.7(2017):2639-2654.
Files in This Item:
File Name/Size DocType Version Access License
Ural Blocking as an (4609KB)期刊论文出版稿开放获取CC BY-NC-SAView Application Full Text
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[Gong, Tingting]'s Articles
[Luo, Dehai]'s Articles
Baidu academic
Similar articles in Baidu academic
[Gong, Tingting]'s Articles
[Luo, Dehai]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Gong, Tingting]'s Articles
[Luo, Dehai]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: Ural Blocking as an Amplifier of the Arctic Sea Ice Decline in Winter.pdf
Format: Adobe PDF
All comments (0)
No comment.
 

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