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The Southern Oscillation / Northern Oscillation Cycle Associated with Sea Surface Temperature in the Equatorial Pacific


doi: 10.1007/BF02658141

  • This paper analyzed the time evolution of the global 1000 hPa height anomalies related to the sea surface tem-perature (SST) in the eastern equatorial Pacific by using ECMWF data in the period 1979-1988, in which two Pacific warm events, 1982/83 and 1986/87, are included. It is found that there are distinct evidences of eastward propaga-tion of alternate positive / negative height anomalies not only in the tropical South Pacific but also in the tropical North Pacific. The former is associated with the Southern Oscillation (SO) and the latter is associated with the so-called Northern Oscillation (NO).It is noteworthy that the alternate positive / negative anomaly centers associated with SO and NO can be traced back to the middle and higher latitudes of the South Indian Ocean and the East Asian continent respectively, which may be significant for the understanding of the causes and mechanism of SO and NO and for the monitoring of ENSO.Furthermore, these evolution processes have a strong symmetry about the Northern and the Southern Hemi-sphere. The whole SO / NO cycle takes about 3.5 years from extreme positive to negative index pattern and again from extreme negative to positive index pattern, It is suggested that the anomalous cold air activities over East Asia and Australia and the polar vortex activities over the northern and the southern Pacific seem to have dominant role on the SO / NO cycle.
  • [1] XU Kang, ZHU Congwen, HE Jinhai, 2013: Two Types of El Nio-related Southern Oscillation and Their Different Impacts on Global Land Precipitation, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1743-1757.  doi: 10.1007/s00376-013-2272-3
    [2] Pavla PEKAROVA, Jan PEKAR, 2007: Teleconnections of Inter-Annual Streamflow Fluctuation in Slovakia with Arctic Oscillation, North Atlantic Oscillation, Southern Oscillation, and Quasi-Biennial Oscillation Phenomena, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 655-663.  doi: 10.1007/s00376-007-0655-z
    [3] LI Gen, REN Baohua, YANG Chengyun, ZHENG Jianqiu, 2010: Indices of El Nino and El Nino Modoki: An improved El Nino Modoki index, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 1210-1220.  doi: 10.1007/s00376-010-9173-5
    [4] Zhang Renhe, Zhao Gang, Tan Yanke, 2001: Meridional Wind Stress Anomalies over Tropical Pacific and the Onset of El Nino. Part Ⅰ: Data Analysis, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 467-480.  doi: 10.1007/s00376-001-0038-9
    [5] YUAN Yuan, ZHOU Wen, YANG Hui, LI Chongyin, 2008: Warming in the Northwestern Indian Ocean Associated with the El Ni\~no Event, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 246-252.  doi: 10.1007/s00376-008-0246-7
    [6] Zhang Renhe, Zhao Gang, 2001: Meridional Wind Stress Anomalies over the Tropical Pacific and the Onset of El Ni?o Part Ⅱ: Dynamical Analysis, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 1053-1065.  doi: 10.1007/s00376-001-0022-4
    [7] Shouhong WANG, MA Tian, 2011: El Nino Southern Oscillation as Sporadic Oscillations between Metastable States, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 612-622.  doi: 10.1007/s00376-010-9089-0
    [8] Fu Congbin, Dong Dongfeng, Ralph Slutz, Joseph Fletcher, 1988: EL NINO/SOUTHERN OSCILLATION SIGNALS IN THE GLOBAL TROPICAL OCEAN, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 35-46.  doi: 10.1007/BF02657344
    [9] Yuan Zhuojian, Jian Maoqiu, 2001: Diagnostic Equations for the Walker Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 166-178.  doi: 10.1007/s00376-001-0011-7
    [10] Lu Riyu, Chan-Su Ryu, Buwen Dong, 2002: Associations between the Western North Pacific Monsoon and the South China Sea Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 12-24.  doi: 10.1007/s00376-002-0030-z
    [11] Li'an Xie, Leonard J.Pietrafesa, Kejian Wu, 2002: Interannual and Decadal Variability of Landfalling Tropical Cyclones in the Southeast Coastal States of the United States, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 677-686.  doi: 10.1007/s00376-002-0007-y
    [12] ZHANG Rong-Hua, ZHENG Fei, PEI Yuhua, ZHENG Quanan, WANG Zhanggui, 2012: Modulation of El Nino-Southern Oscillation by Freshwater Flux and Salinity Variability in the Tropical Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 647-660.  doi: 10.1007/s00376-012-1235-4
    [13] Wang Huijun, 1999: A Preliminary Study on the Polar Climate Predictability, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 361-366.  doi: 10.1007/s00376-999-0015-2
    [14] K.D. Prasad, S.V. Singh, 1988: MONSOON RAINFALL AND SOUTHERN OSCILLATION RESPONSES IN THE PRESSURES OVER THE NORTHERN INDIAN OCEAN, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 243-251.  doi: 10.1007/BF02656785
    [15] ZHOU Yang, JIANG Jing, Youyu LU, and HUANG Anning, 2013: Revealing the effects of the El Nio-Southern oscillation on tropical cyclone intensity over the western North Pacific from a model sensitivity study, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1117-1128.  doi: 10.1007/s00376-012-2109-5
    [16] Shi Neng, 1988: A MULTI-STATISTICAL ANALYSIS OF THE SOUTHERN OSCILLATION (SO) AND ITS RELATION TO THE MEAN MONTHLY ATMOSPHERIC CIRCULATION AT 500 hPa IN THE NORTHERN HEMISPHERE, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 345-360.  doi: 10.1007/BF02656758
    [17] YUAN Wei, SUN Jianqi, 2009: Enhancement of the Summer North Atlantic Oscillation Influence on Northern Hemisphere Air Temperature, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 1209-1214.  doi: 10.1007/s00376-009-8148-x
    [18] Chen Lieting, 1985: THE SOUTHERN OSCILLATION AND ITS ASSOCIATEDSUMMER RAINFALLS IN CHINA-CONCURRENTDISCUSSION OF THE RELATIONSHIP BETWEEN THE SOURTHERN OSCILLATION AND WALKER CIRCULATION, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 542-548.  doi: 10.1007/BF02678752
    [19] Xiaomeng SONG, Renhe ZHANG, Xinyao RONG, 2019: Influence of Intraseasonal Oscillation on the Asymmetric Decays of El Niño and La Niña, ADVANCES IN ATMOSPHERIC SCIENCES, , 779-792.  doi: 10.1007/s00376-019-9029-6
    [20] Liu Jianwen, Dong Peiming, 2001: Short-range Climate Prediction Experiment of the Southern Oscillation Index Based on the Singular Spectrum Analysis, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 873-881.

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Manuscript History

Manuscript received: 10 July 1993
Manuscript revised: 10 July 1993
通讯作者: 陈斌, bchen63@163.com
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The Southern Oscillation / Northern Oscillation Cycle Associated with Sea Surface Temperature in the Equatorial Pacific

  • 1. Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080

Abstract: This paper analyzed the time evolution of the global 1000 hPa height anomalies related to the sea surface tem-perature (SST) in the eastern equatorial Pacific by using ECMWF data in the period 1979-1988, in which two Pacific warm events, 1982/83 and 1986/87, are included. It is found that there are distinct evidences of eastward propaga-tion of alternate positive / negative height anomalies not only in the tropical South Pacific but also in the tropical North Pacific. The former is associated with the Southern Oscillation (SO) and the latter is associated with the so-called Northern Oscillation (NO).It is noteworthy that the alternate positive / negative anomaly centers associated with SO and NO can be traced back to the middle and higher latitudes of the South Indian Ocean and the East Asian continent respectively, which may be significant for the understanding of the causes and mechanism of SO and NO and for the monitoring of ENSO.Furthermore, these evolution processes have a strong symmetry about the Northern and the Southern Hemi-sphere. The whole SO / NO cycle takes about 3.5 years from extreme positive to negative index pattern and again from extreme negative to positive index pattern, It is suggested that the anomalous cold air activities over East Asia and Australia and the polar vortex activities over the northern and the southern Pacific seem to have dominant role on the SO / NO cycle.

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