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Volume 5 Issue 4

Oct.  1988

Article Contents

TELECONNECTION OF THE DOMINANT SPATIAL PATTERNS OF THE SEASONAL 500 hPa GPH FIELD


doi: 10.1007/BF02656788

  • The dominant spatial patterns of the seasonal 500 hPa GPH field is induced by the EOF analysis. In winter, the first and fourth eigenvector show that the PEA and PNA-like anomalous flow pattern will prevail when the temporal coefficient is negative. Through the variation of the temporal coefficient of the eigen-vector, prevailing of these flow patterns is significantly related to the variation of SST in equatorial Pacific. These relationships are insignificant in other three seasons.
  • [1] Chen Yingyi, 1993: Predictability of the 500 hPa Height Field, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 497-503.  doi: 10.1007/BF02656975
    [2] Wang Panxing, Gao Zhi, Li Changqing, 1987: ANALYSIS OF THE TELECONNECTIONAL STRUCTURES OF THE 500-hPa HEIGHT FIELD OVER THE NH IN JANUARY, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 185-197.  doi: 10.1007/BF02677065
    [3] Qiu Yongyan, 1993: On the Seasonal Transition and the Interannual Variability in Global Kinetic Energy at 500 hPa, Accompanied with Anomalies of Energy during the 1982 / 83 ENSO, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 248-256.  doi: 10.1007/BF02919148
    [4] Ji Zhengang, Chao Jiping, 1987: TELECONNECTIONS OF THE SEA SURFACE TEMPERATURE IN THE INDIAN OCEAN WTTH SEA SURFACE TEMPERATURE IN THE EASTERN EQUATORIAL PACIFIC, AND WITH THE 500 hPa GEOPOTENTIAL HEIGHT FIELD IN THE NORTHERN HEMISPHERE, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 343-348.  doi: 10.1007/BF02663604
    [5] Li Zhijin, Ji Liren, 1996: Internal Dynamics of the Generation of Atmospheric Teleconnection Patterns, ADVANCES IN ATMOSPHERIC SCIENCES, 13, 19-32.  doi: 10.1007/BF02657025
    [6] Xue Feng, Zeng Qingcun, 1997: Teleconnection Patterns in the Northern Hemisphere Simulated by IAP GCM, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 41-48.  doi: 10.1007/s00376-997-0041-x
    [7] Fang Zhifang, John M. Wallace, David W. J. Thompson, 2001: The Relationship between the Meridional Profile of Zonal mean Geostrophic Wind and Station Wave at 500 hPa, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 692-700.
    [8] S. V. Singh, S. R. Inamdar, R. H. Kripalani, K. D. Prasad, 1986: RELATIONSHIP BETWEEN 500 hPa RIDGE AXIS POSITIONS OVER THE INDIAN AND THE WEST PACIFIC REGIONS AND THE INDIAN SUMMER MONSOON RAINFALL, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 349-359.  doi: 10.1007/BF02678655
    [9] Shi Neng, Luo Boliang, 1991: Telecorrelation of the 500 hPa Polar Circulation and El Nino / SO with the Temperature Fields in China, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 289-298.  doi: 10.1007/BF02919611
    [10] Iman ROUSTA, Mehdi DOOSTKAMIAN, Esmaeil HAGHIGHI, Hamid Reza GHAFARIAN MALAMIRI, Parvane YARAHMADI, 2017: Analysis of Spatial Autocorrelation Patterns of Heavy and Super-Heavy Rainfall in Iran, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 1069-1081.  doi: 10.1007/s00376-017-6227-y
    [11] ZHENG Bin, GU Dejun, LIN Ailan, LI Chunhui, 2008: Spatial Patterns of Tropospheric Biennial Oscillation and Its Numerical Simulation, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 815-823.  doi: 10.1007/s00376-008-0815-9
    [12] CHEN Boyu, MU Mu, 2012: The Roles of Spatial Locations and Patterns of Initial Errors in the Uncertainties of Tropical Cyclone Forecasts, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 63-78.  doi: 10.1007/s00376-011-0201-x
    [13] LI Gang, LI Chongyin, TAN Yanke, BAI Tao, 2012: Seasonal Evolution of Dominant Modes in South Pacific SST and Relationship with ENSO, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 1238-1248.  doi: 10.1007/s00376-012-1191-z
    [14] 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
    [15] Chen Wanlong, Chu Pao-Shin, 1990: On the Couplings between Chebyshev Coefficients as Derived from the Monthly Mean Geopotential Fields at 500 hPa over East Asia and the Southern Oscillation, ADVANCES IN ATMOSPHERIC SCIENCES, 7, 347-353.  doi: 10.1007/BF03179766
    [16] YE Hong, LU Riyu, 2012: Dominant Patterns of Summer Rainfall Anomalies in East China during 1951--2006, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 695-704.  doi: 10.1007/s00376-012-1153-5
    [17] GAO Shouting, YANG Shuai, XUE Ming, CUI Chunguang, 2008: Total Deformation and its Role in Heavy Precipitation Events Associated with Deformation-Dominant Flow Patterns, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 11-23.  doi: 10.1007/s00376-008-0011-y
    [18] Hoffman H. N. CHEUNG, Wen ZHOU, 2016: Simple Metrics for Representing East Asian Winter Monsoon Variability: Urals Blocking and Western Pacific Teleconnection Patterns, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 695-705.  doi: 10.1007/s00376-015-5204-6
    [19] Shi Neng, Zhu Qiangen, 1993: Studies on the Northern Early Summer Teleconnection Patterns, Their Interannual Variations and Relation to Drought / Flood in China, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 155-168.  doi: 10.1007/BF02919138
    [20] SONG Lianchun, A. J. CANNON, P. H. WHITFIELD, 2007: Changes in Seasonal Patterns of Temperature and Precipitation in China During 1971--2000, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 459-473.  doi: 10.1007/s00376-007-0459-1

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Manuscript History

Manuscript received: 10 October 1988
Manuscript revised: 10 October 1988
通讯作者: 陈斌, bchen63@163.com
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TELECONNECTION OF THE DOMINANT SPATIAL PATTERNS OF THE SEASONAL 500 hPa GPH FIELD

  • 1. Institute of Atmospheric Physics, Academia Sinica, Beijing

Abstract: The dominant spatial patterns of the seasonal 500 hPa GPH field is induced by the EOF analysis. In winter, the first and fourth eigenvector show that the PEA and PNA-like anomalous flow pattern will prevail when the temporal coefficient is negative. Through the variation of the temporal coefficient of the eigen-vector, prevailing of these flow patterns is significantly related to the variation of SST in equatorial Pacific. These relationships are insignificant in other three seasons.

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