DOI: 10.1002/joc.5461
论文题名: Pacific multi-decadal oscillation modulates the effect of Arctic oscillation and El Niño southern oscillation on the East Asian winter monsoon
作者: Chen D. ; Wang H. ; Sun J. ; Gao Y.
刊名: International Journal of Climatology
ISSN: 8998418
出版年: 2018
卷: 38, 期: 6 起始页码: 2808
结束页码: 2818
语种: 英语
英文关键词: Arctic oscillation
; Asia-Pacific region
; EAWM
; ENSO
; inter-decadal change
Scopus关键词: Atmospheric pressure
; Atmospheric thermodynamics
; Fluxes
; Oceanography
; Surface waters
; Arctic Oscillation
; Asia Pacific region
; EAWM
; ENSO
; Interdecadal
; Climatology
; Arctic Oscillation
; decadal variation
; El Nino-Southern Oscillation
; monsoon
; Pacific Decadal Oscillation
; prediction
; regional climate
; sea surface temperature
; winter
; Bering Strait
; Pacific Ocean
; Pacific Rim
英文摘要: In this study, the relationship between the East Asian winter monsoon (EAWM) and the Arctic oscillation (AO) and El Niño southern oscillation (ENSO) are reanalysed using long-term reanalysis data. The AO and ENSO influence the EAWM by means of a significant inter-decadal oscillation with a periodicity of approximately 60 years. When the linkage between the AO and EAWM is strengthened (weakened), the ENSO has a weakened (strengthened) relationship with the EAWM. The AO and ENSO alternately affect the EAWM for approximately 30 years. Furthermore, an analysis is completed regarding the possible mechanism of the inter-decadal relationship between the EAWM and ENSO, as well as the AO. Such an inter-decadal relationship could be due to the phase transition of the Pacific multi-decadal oscillation (PMO). When the PMO is positive, sea surface temperatures (SSTs) in the Bering Strait and Alaska Current region are warmer than average, which results in a decrease in the East Asian trough and an increase in the Aleutian low and northeastern Pacific vertical wave activity flux. In this case, the vertical wave activity flux propagates upward and is reflected in the polar vortex, which significantly strengthens the relationship between the Asia-Pacific climate and AO. Simultaneously, during the positive phase of the PMO, the increase in the SST in the eastern South Pacific is stronger than in the west, which leads to a weakening of the east–west temperature gradient and southern oscillation. Thus, the relationship between the ENSO and Asia-Pacific region is significantly weakened and vice versa. The results of this study deepen the understanding of the Asia-Pacific climate and may improve the inter-decadal prediction of the Asia-Pacific regional climate in the future. © 2018 Royal Meteorological Society Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/116900
Appears in Collections: 气候减缓与适应
There are no files associated with this item.
作者单位: Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China; Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology, Nanjing, China; Climate Change Research Center, Chinese Academy of Sciences, Beijing, China; University of Chinese Academy of Sciences, Beijing, China
Recommended Citation:
Chen D.,Wang H.,Sun J.,et al. Pacific multi-decadal oscillation modulates the effect of Arctic oscillation and El Niño southern oscillation on the East Asian winter monsoon[J]. International Journal of Climatology,2018-01-01,38(6)