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On the significance of the interannual relationship between the Asian‐Pacific Oscillation and the North Atlantic Oscillation
Author(s) -
Zhou Botao,
Wang Zunya
Publication year - 2015
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2015jd023328
Subject(s) - anticyclone , climatology , north atlantic oscillation , teleconnection , anomaly (physics) , geopotential height , empirical orthogonal functions , pacific decadal oscillation , troposphere , atmospheric circulation , atlantic multidecadal oscillation , geology , oceanography , sea surface temperature , geography , el niño southern oscillation , precipitation , meteorology , physics , condensed matter physics
Using monthly data from the European Centre for Medium‐Range Weather Forecasts 40 year Re‐Analysis, this study investigated the interannual relationship between the Asian‐Pacific Oscillation (APO) and the North Atlantic Oscillation (NAO) for the period of May to August. The NAO is represented by the leading Empirical Orthogonal Function of sea level pressure anomalies over the Atlantic sector. The difference of upper tropospheric eddy air temperature ( T ′) between Asia and the North Pacific is used to measure the APO. Results clearly show that the APO and the NAO correlated very well on the interannual time scale, with the positive (negative) phase of the APO corresponding to the strong (weak) NAO. Such a relationship is well supported by the atmospheric dynamic process. When the APO is in the positive phase (characterized by the positive T ′ anomaly over Asia and the negative T ′ anomaly over the North Pacific in the upper troposphere), the upper tropospheric geopotential height increases over Asia and decreases over the North Pacific. Accordingly, anticyclonic circulation and cyclonic circulation anomalies are introduced, respectively, over Asia and south of the North Pacific, and a zonal teleconnection wave train is excited from Asia to the North Atlantic. As a consequence, an anomalous anticyclonic circulation prevails in the low level of the North Atlantic and an anomalous cyclonic circulation appears to its north, which corresponds to the atmospheric pattern of strong NAO. Further study proposes that the quasi‐stationary wave pattern emanating from the western North Pacific region may serve as a bridge for this linkage.