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Volume 9 Issue 1

Jan.  1992

Article Contents

The Propagation of Inertia-Gravity Waves and Their Influence on Zonal Mean Flow Part Two: Wave Breaking and Critical Levels


doi: 10.1007/BF02656927

  • The gravity wave breaking is crucial to the large-scale circulation of middle atmosphere. In this paper, we follow Lindzen (1981) to draw out the parameterization of two-dimensional gravity wave breaking including inertial effect. Also we present some properties of critical levels and inertial critical levels.
  • [1] Zheng Xingyu, Zeng Qingcun, Huang Ronghui, 1991: The Propagation of Inertia-Gravity Waves and Their Influence on Mean Zonal Flow, Part One: the Propagation of Inertia-Gravity Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 431-446.  doi: 10.1007/BF02919266
    [2] Lu LIU, Lingkun RAN, Shouting GAO, 2019: A Three-dimensional Wave Activity Flux of Inertia-Gravity Waves and Its Application to a Rainstorm Event, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 206-218.  doi: 10.1007/s00376-018-8018-5
    [3] Lu LIU, Lingkun RAN, Shouting GAO, 2018: Analysis of the Characteristics of Inertia-Gravity Waves during an Orographic Precipitation Event, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 604-620.  doi: 10.1007/s00376-017-7159-2
    [4] Zhu Xun, 1987: ON GRAVITY WAVE-MEAN FLOW INTERACTIONS IN A THREE DIMENSIONAL STRATIFIED ATMOSPHERE, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 287-299.  doi: 10.1007/BF02663599
    [5] Zhao Ping, 1991: The Effects of Zonal Flow on Nonlinear Rossby Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 299-306.  doi: 10.1007/BF02919612
    [6] He Jianzhong, 1993: Topography and the Non-linear Rossby Wave in the Zonal Shear Basic Flow, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 233-242.  doi: 10.1007/BF02919146
    [7] 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
    [8] Zeng Qingcun, Zhang Minghua, 2000: Wave-Mean Flow Interaction: the Role of Continuous-Spectrum Disturbances, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 1-17.  doi: 10.1007/s00376-000-0039-0
    [9] LIU Chengji, REN Xuejuan*, and YANG Xiuqun, 2014: Mean FlowStorm Track Relationship and RossbyWave Breaking in Two Types of El-Nio, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 197-210.  doi: 10.1007/s00376-013-2297-7
    [10] CHEN Bomin, JI Liren, YANG Peicai, ZHANG Daomin, 2003: Systematic Errors of Zonal-Mean Flow in Dynamical Monthly Prediction and Its Improvement, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 17-27.  doi: 10.1007/BF03342046
    [11] Wu Guoxiong, Chen Biao, 1989: Non-Acceleration Theorem in a Primitive Equation System: I. Acceleration of Zonal Mean Flow, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 1-20.  doi: 10.1007/BF02656914
    [12] 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.
    [13] LI Xiaofeng, LI Jianping, Xiangdong ZHANG, 2013: A Two-way Stratosphere-Troposphere Coupling of Submonthly Zonal-Mean Circulations in the Arctic, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1771-1785.  doi: 10.1007/s00376-013-2210-4
    [14] Xiaofan Li, Han-Ru Cho, 1997: Development and Propagation of Equatorial Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 323-338.  doi: 10.1007/s00376-997-0053-6
    [15] 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
    [16] Zeng Qingcun, Lu Peisheng, Li Rongfeng, Yuan Chongguang, 1986: EVOLUTION OF LARGE SCALE DISTURBANCES AND THEIR INTERACTION WITH MEAN FLOW IN A ROTATING BAROTROPIC ATMOSPHERE PART II, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 172-188.  doi: 10.1007/BF02680044
    [17] Zeng Qingcun, Lu Peisheng, Li Rongfeng, Yuan Chongguang, 1986: EVOLUTION OF LARGE SCALE DISTURBANCES AND THEIR INTERACTION WITH MEAN FLOW IN A ROTATING BAROTROPIC ATMOSPHERE —PART I, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 39-58.  doi: 10.1007/BF02682551
    [18] Sun Shuqing, 1985: GRAVITY WAVES ON THE AXIS OF LOW LEVEL JET AND THEIR INSTABILITY, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 112-123.  doi: 10.1007/BF03179743
    [19] Zhang Ying, Shen Xinyong, Zhang Ming, 1990: Analysis and Study of a Mesoscale Inertia-Gravitational Wave in Upper Air, ADVANCES IN ATMOSPHERIC SCIENCES, 7, 220-226.  doi: 10.1007/BF02919160
    [20] Shen Xinyong, Ni Yunqi, Ding Yihui, 2002: On Problem of Nonlinear Symmetric Instability in Zonal Shear Flow, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 350-364.  doi: 10.1007/s00376-002-0027-7

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Manuscript History

Manuscript received: 10 January 1992
Manuscript revised: 10 January 1992
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 Propagation of Inertia-Gravity Waves and Their Influence on Zonal Mean Flow Part Two: Wave Breaking and Critical Levels

  • 1. Institute of Atmospheric Physics, Academia Sinica, Beijing 100080,Institute of Atmospheric Physics, Academia Sinica, Beijing 100080,Institute of Atmospheric Physics, Academia Sinica, Beijing 100080

Abstract: The gravity wave breaking is crucial to the large-scale circulation of middle atmosphere. In this paper, we follow Lindzen (1981) to draw out the parameterization of two-dimensional gravity wave breaking including inertial effect. Also we present some properties of critical levels and inertial critical levels.

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