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DOI | 10.1175/JCLI-D-18-0283.1 |
Differences in the Silk Road Pattern and Its Relationship to the North Atlantic Oscillation between Early and Late Summers | |
Hong, Xiaowei1,2; Lu, Riyu3,4; Li, Shuanglin1,2,5 | |
2018-11-01 | |
发表期刊 | JOURNAL OF CLIMATE
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ISSN | 0894-8755 |
EISSN | 1520-0442 |
出版年 | 2018 |
卷号 | 31期号:22页码:9283-9292 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
英文摘要 | The Silk Road Pattern (SRP) is an upper-tropospheric teleconnection pattern along the Asian westerly jet in summer on the interannual time scale, and it exerts great influences on the climate of the Eurasian continent. Results in the present study indicate that the SRP exhibits considerable distinctions between early and late summers (i.e., 1 June-9 July and 10 July-31 August, respectively). The SRP is stronger and more geographically fixed in late summer in comparison with its counterpart in early summer. Furthermore, the SRP is closely connected with the summer North Atlantic Oscillation (SNAO) in late summer, but not in early summer. This closer connection in late summer is manifested clearly in the leading mode of upper-tropospheric meridional wind anomalies over the North Atlantic-Eurasian continent domain. The intensified SNAO-SRP relationship in late summer can be explained by the subseasonal change of the SNAO: albeit being a seesaw pattern common in both early and late summers, there is a shift of this pattern toward the northwest-southeast one in late summer from a north-south one in early summer. The southeastern pole of SNAO in late summer extends into the Eurasian continent, and efficiently triggers the SRP to propagate along the Asian jet. By contrast, the south pole of SNAO in early summer is confined over the North Atlantic and is thus less effective to trigger the SRP propagation. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000450830400001 |
WOS关键词 | ROSSBY-WAVE PROPAGATION ; CIRCUMGLOBAL TELECONNECTION ; EURASIAN CONTINENT ; MODEL SIMULATIONS ; YANGTZE-RIVER ; LATE 1970S ; ASIAN JET ; PRECIPITATION ; RAINFALL ; SEESAW |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/20236 |
专题 | 气候变化 |
作者单位 | 1.Chinese Acad Sci, Inst Atmospher Phys, Climate Change Res Ctr, Beijing, Peoples R China; 2.Chinese Acad Sci, Inst Atmospher Phys, Nansen Zhu Int Res Ctr, Beijing, Peoples R China; 3.Chinese Acad Sci, State Key Lab Numer Modeling Atmospher Sci & Geop, Inst Atmospher Phys, Beijing, Peoples R China; 4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China; 5.China Univ Geosci, Sch Environm Studies, Dept Atmospher Sci, Wuhan, Hubei, Peoples R China |
推荐引用方式 GB/T 7714 | Hong, Xiaowei,Lu, Riyu,Li, Shuanglin. Differences in the Silk Road Pattern and Its Relationship to the North Atlantic Oscillation between Early and Late Summers[J]. JOURNAL OF CLIMATE,2018,31(22):9283-9292. |
APA | Hong, Xiaowei,Lu, Riyu,&Li, Shuanglin.(2018).Differences in the Silk Road Pattern and Its Relationship to the North Atlantic Oscillation between Early and Late Summers.JOURNAL OF CLIMATE,31(22),9283-9292. |
MLA | Hong, Xiaowei,et al."Differences in the Silk Road Pattern and Its Relationship to the North Atlantic Oscillation between Early and Late Summers".JOURNAL OF CLIMATE 31.22(2018):9283-9292. |
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