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Volume 17 Issue 2

Apr.  2000

Article Contents
Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 2000 >  17(2): 311-321

Low-Frequency CISK-Rossby Wave and Stratospheric QBO in the Tropical Atmosphere

  • 1.

    Institute of Meteorology, PLA University of Science and Technology, Nanjing 211101,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093


doi: 10.1007/s00376-000-0012-y

  • Dynamic study is undertaken of the tropical atmospheric CISK-Rossby wave genesis and propagation mechanisms, the vertical structure of the low-frequency wave and the basic characteristics and constraint of the vertical transport of momentum and wave energy fluxes in relation to the quasi-biennial oscillation (QBO) of the stratospheric zonal winds over the tropics in the context of a baroclinic quasi-geoslrophic model. Results suggest that in the properly posed thermal conditions and zonal belt there exist two kinds of CISK-Rossby waves of low frequency (LF) and very low frequency (VLF), travelling zonally in opposite di-rections, which act as sources responsible for upward transferring momentum and wave energy fluxes for easterly and westerly perturbations in such a way as to provide required momentum and energy for the stratospheric QBO genesis and maintenance. The present study offers interpretations for some of the fun-damental observational facts of the QBO and proposes mew ideas of the QBO generation mechanism.
  • [1] Liao Qinghai, Li Chongyin, 1995: CISK-rossby wave and the 30-60 Day Oscillation in the Tropics, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 1-12.  doi: 10.1007/BF02661282
    [2] CHEN Gong, and LI Guoping, 2014: Dynamic and Numerical Study of Waves in the Tibetan Plateau Vortex, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 131-138.  doi: 10.1007/s00376-013-1035-5
    [3] Zhang Daizhou, Tanaka Hiroshi, Qin Yu, 1996: Internal Gravity Waves Generated by a Local Thermal Source in an Irrotational Zonal-Vertical Plane: Numerical Analysis, ADVANCES IN ATMOSPHERIC SCIENCES, 13, 124-132.  doi: 10.1007/BF02657033
    [4] Jiang Guorong, 1996: CISK-related Rossby Waves in the Tropical Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 13, 115-123.  doi: 10.1007/BF02657032
    [5] Hengyi WENG, 2003: Impact of the 11-yr Solar Activity on the QBO in the Climate System, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 303-309.  doi: 10.1007/s00376-003-0017-4
    [6] CHEN Wen, WEI Ke, 2009: Interannual Variability of the Winter Stratospheric Polar Vortex in the Northern Hemisphere and their Relations to QBO and ENSO, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 855-863.  doi: 10.1007/s00376-009-8168-6
    [7] Zou Han, Ji Chongping, Zhou Libo, 2000: QBO Signal in Total Ozone over Tibet, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 562-568.  doi: 10.1007/s00376-000-0019-4
    [8] Zhang Ren, Yu Zhihao, 2000: Numerical and Dynamical Analyses of Heat Source Forcing and Restricting Subtropical High Activity, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 61-71.  doi: 10.1007/s00376-000-0043-4
    [9] Qiwei WANG, Ming XUE, Zhemin TAN, 2016: Convective Initiation by Topographically Induced Convergence Forcing over the Dabie Mountains on 24 June 2010, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 1120-1136.  doi: 10.1007/s00376-016-6024-z
    [10] DUAN Anmin, WU Guoxiong, LIANG Xiaoyun, 2008: Influence of the Tibetan Plateau on the Summer Climate Patterns over Asia in the IAP/LASG SAMIL Model, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 518-528.  doi: 10.1007/s00376-008-0518-2
    [11] Bian Jianchun, Chen Hongbin, Zhao Yanliang, Lü Daren, 2002: Variation Features of Total Atmospheric Ozone in Beijing and Kunming Based on Dobson and TOMS Data, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 279-286.  doi: 10.1007/s00376-002-0022-z
    [12] A.B. Sikder, S.K. Patwardhan, H.N. Bhalme, 1993: Tropical Stratospheric Circulation and Monsoon Rainfall, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 379-385.  doi: 10.1007/BF02658143
    [13] Zhang Daizhou, Qin Yu, 1995: QBO-like Oscillations Induced by Local Thermal Forcing, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 245-254.  doi: 10.1007/BF02656837
    [14] WANG Lu, and YANG Haijun, 2014: The Role of Atmospheric Teleconnection in the Subtropical Thermal Forcing on the Equatorial Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 985-994.  doi: 10.1007/s00376-013-3173-1
    [15] Zhang Qin, Zhu Yufeng, Ni Yunqi, 1995: QBO Features of Tropical Pacific wind Stress Field with the Relation to El Nino, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 87-94.  doi: 10.1007/BF02661290
    [16] CHEN Yuejuan, SHI Chunhua, ZHENG Bin, 2005: HCl Quasi-Biennial Oscillation in the Stratosphere and a Comparison with Ozone QBO, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 751-758.  doi: 10.1007/BF02918718
    [17] Fukai LIU, Yiyong LUO, Jian LU, Xiuquan WAN, 2021: The Role of Ocean Dynamics in the Cross-equatorial Energy Transport under a Thermal Forcing in the Southern Ocean, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 1737-1749.  doi: 10.1007/s00376-021-1099-6
    [18] Qin Jianchun, Zhu Baozhen, 1986: A STUDY ON THE EXCITATION, ESTABLISHMENT AND TRANSITION OF MULTIPLE EQUILIBRIUM STATES PRODUCED BY NEARLY RESONANT THERMAL FORCING---- PART I: ASYMPTOTIC SOLUTIONS　OF MULTIPLE EQUILIBRIUM STATES, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 277-288.  doi: 10.1007/BF02678649
    [19] Li Liming, Huang Feng, Chi Dongyan, Liu Shikuo, Wang Zhanggui, 2002: Thermal Effects of the Tibetan Plateau on Rossby Waves from the Diabatic Quasi-Geostrophic Equations of Motion, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 901-913.  doi: 10.1007/s00376-002-0054-4
    [20] Huang Ronghui, Wang Lianying, 1990: Relationship between the Interannual Variations of Total Ozone in the Northern Hemisphere and the QBO of Basic Flow in the Tropical Stratosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 7, 47-56.  doi: 10.1007/BF02919167
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    • Manuscript History

    Manuscript received: 10 April 2000
    Manuscript revised: 10 April 2000
    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

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    Low-Frequency CISK-Rossby Wave and Stratospheric QBO in the Tropical Atmosphere

    • 1. Institute of Meteorology, PLA University of Science and Technology, Nanjing 211101,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093
    • Manuscript received: 2000-04-10
    • Manuscript revised: 2000-04-10

    Abstract: Dynamic study is undertaken of the tropical atmospheric CISK-Rossby wave genesis and propagation mechanisms, the vertical structure of the low-frequency wave and the basic characteristics and constraint of the vertical transport of momentum and wave energy fluxes in relation to the quasi-biennial oscillation (QBO) of the stratospheric zonal winds over the tropics in the context of a baroclinic quasi-geoslrophic model. Results suggest that in the properly posed thermal conditions and zonal belt there exist two kinds of CISK-Rossby waves of low frequency (LF) and very low frequency (VLF), travelling zonally in opposite di-rections, which act as sources responsible for upward transferring momentum and wave energy fluxes for easterly and westerly perturbations in such a way as to provide required momentum and energy for the stratospheric QBO genesis and maintenance. The present study offers interpretations for some of the fun-damental observational facts of the QBO and proposes mew ideas of the QBO generation mechanism.

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