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Volume 3 Issue 4

Oct.  1986

Article Contents

THE NONLINEAR INTERACTION BETWEEN DIFFERENT WAVE COMPONENTS AND THE PROCESS OF INDEX CYCLE OF GENERAL CIRCULATION


doi: 10.1007/BF02657937

  • By using a two-level quasi-geostrophic truncated spectral model taking account of the nonlinear in-teraction between different wave components (i. e. basic current, ultra-long waves and long waves), the index cycle of general circulation is investigated. The calculated results show that the circulation index has a, quasi-periodic vacillation with a period of 8 to 16 days, which can be created by the nonlinear interaction and that the nonlinear interaction between different wave components may cause the tilted-trough vacillation, amplitude vacillation of wave pattern and quasi-periodic change of wave number of flow pattern.
  • [1] Hu Zengzhen, Tsuyoshi Nitta, 1997: Seasonality of the Interaction between Convection over the Western Pacific and General Circulation in the Northern Hemisphere, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 541-553.  doi: 10.1007/s00376-997-0072-3
    [2] XUN Xueyi, HU Zeyong, MA Yaoming, 2012: The Dynamic Plateau Monsoon Index and Its Association with General Circulation Anomalies, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 1249-1263.  doi: 10.1007/s00376-012-1125-9
    [3] M. Sankar-Rao, V. N. Lykossov, E. M. Volodin, A. E. Nikitin, A. I. Degtiarev, Kusuma G. Rao, 1991: Relationships between the Global General Circulation and the Indian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 137-148.  doi: 10.1007/BF02658090
    [4] Gao Shouting, 1991: A-B Hybrid Equation Method of Nonlinear Bifurcation in Wave-Flow Interaction, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 165-174.  doi: 10.1007/BF02658092
    [5] Luo Dehai, 1999: Nonlinear Three-Wave Interaction among Barotropic Rossby Waves in a Large-scale Forced Barotropic Flow, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 451-466.  doi: 10.1007/s00376-999-0023-2
    [6] Li Chongyin, Sun Shuqing, Mu Mingquan, 2001: Origin of the TBO-Interaction between Anomalous East-Asian Winter Monsoon and ENSO Cycle, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 554-566.  doi: 10.1007/s00376-001-0044-y
    [7] HUANG Ronghui, CHEN Wen, YANG Bangliang, ZHANG Renhe, 2004: Recent Advances in Studies of the Interaction between the East Asian Winter and Summer Monsoons and ENSO Cycle, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 407-424.  doi: 10.1007/BF02915568
    [8] LUO Dehai, LIU Jinting, LI Jianping, 2010: Interaction between Planetary-Scale Diffluent Flow and Synoptic-Scale Waves During the Life Cycle of Blocking, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 807-831.  doi: 10.1007/s00376-009-9074-7
    [9] Zhao Shengju, 1986: RELATION BETWEEN LONG-DISTANCE MIGRATION OF ORIENTAL ARMYWORMS AND SEASONAL VARIATION OF GENERAL CIRCULATION OVER EAST ASIA, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 215-226.  doi: 10.1007/BF02682555
    [10] HAN Bo, LU Shihua, AO Yinhuan, 2010: Analysis on the Interaction between Turbulence and Secondary Circulation of the Surface Layer at Jinta Oasis in Summer, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 605-620.  doi: 10.1007/s00376-009-9015-5
    [11] Zhu Qiangen, He Jinhai, Wang Panxing, 1986: A STUDY OF CIRCULATION DIFFERENCES BETWEEN EAST-ASIAN AND INDIAN SUMMER MONSOONS WITH THEIR INTERACTION, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 466-477.  doi: 10.1007/BF02657936
    [12] Zhang Pei, Ni Yunqi, 1991: Effect of Nonlinear Dynamic Process on Formation and Breakdown of Blocking, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 41-50.  doi: 10.1007/BF02657363
    [13] Yong. L. McHall, 1992: Nonlinear Planetary Wave Instability and Blocking, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 173-190.  doi: 10.1007/BF02657508
    [14] Li Xianlang, 1988: NONLINEAR RESONANCE INTERACTIONS AND INDEX CYCLES IN THE ATMOSPHERE, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 253-264.  doi: 10.1007/BF02656750
    [15] Wang Panxing, Liu Dai, Pan Deyu, 1987: WAVE BOUNDARY BETWEEN MIDDLE-AND-LOW AND MIDDLE-AND-HIGH LATITUDE CIRCULATIONS, AND SEASONAL TRANSFORMATION OF NORTHERN-HEMISPHERE MEAN CIRCULATION, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 55-65.  doi: 10.1007/BF02656661
    [16] Luo Dehai, Li Jianping, 2001: Interaction between a Slowly Moving Planetary-Scale Dipole Envelope Rossby Soliton and a Wavenumber-Two Topography in a Forced Higher Order Nonlinear Schr dinger Equation, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 239-256.  doi: 10.1007/s00376-001-0017-1
    [17] Zhang Xuehong, 1985: THE SECOND ORDER APPROXIMATION TO THE NONLINEAR WAVE IN BAROTROPIC ATMOSPHERE, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 167-177.  doi: 10.1007/BF03179749
    [18] R. Dhar, C. Guha-Roy, D. K. Sinha, 1991: On a Class of Solitary Wave Solutions of Atmospheric Nonlinear Equations, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 357-362.  doi: 10.1007/BF02919618
    [19] He Jianzhong, 1994: Nonlinear Ultra-Long Wave and Its Stability, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 91-100.  doi: 10.1007/BF02656998
    [20] Chen Lianshou, Luo Zhexian, 1995: Effect of the Interaction of Different Scale Vortices on the Structure and Motion of Typhoons, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 207-214.  doi: 10.1007/BF02656833

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Manuscript History

Manuscript received: 10 October 1986
Manuscript revised: 10 October 1986
通讯作者: 陈斌, bchen63@163.com
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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THE NONLINEAR INTERACTION BETWEEN DIFFERENT WAVE COMPONENTS AND THE PROCESS OF INDEX CYCLE OF GENERAL CIRCULATION

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

Abstract: By using a two-level quasi-geostrophic truncated spectral model taking account of the nonlinear in-teraction between different wave components (i. e. basic current, ultra-long waves and long waves), the index cycle of general circulation is investigated. The calculated results show that the circulation index has a, quasi-periodic vacillation with a period of 8 to 16 days, which can be created by the nonlinear interaction and that the nonlinear interaction between different wave components may cause the tilted-trough vacillation, amplitude vacillation of wave pattern and quasi-periodic change of wave number of flow pattern.

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