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Volume 1 Issue 1

Jan.  1984

Article Contents

ON THE GENERATION AND MAINTENANCE OF ATMOSPHERIC DISTURBANCES


doi: 10.1007/BF03187611

  • Blocking is one of the intensive atmospheric disturbances which can maintain for a long time. In this paprer we investigate the general conditions favorable for the generation and maintenance of the intensive disturbances. First, the evolutional process of disturbances superimposed on a jet-like zonal flow is studied by using the wave-packet representation and the WKBJ method. Second, the mechanism for generation and maintenance of disturbances is investigated by using the nonlinear equations and the general physical laws. Finally, some numerical experiments are given for illustration, showing the rapid absorption of disturbances by the jet-like zonal flow in one case and the maintenance of disturbances for a long time in the other case.
  • [1] 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
    [2] Su Jeong LEE, Myoung-Hwan AHN, Yeonjin LEE, 2016: Application of an Artificial Neural Network for a Direct Estimation of Atmospheric Instability from a Next-Generation Imager, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 221-232.  doi: 10.1007/s00376-015-5084-9
    [3] Li Chongying, 1985: A NUMERICAL SIMULATION OF TYPHOON GENERATION, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 72-80.  doi: 10.1007/BF03179739
    [4] Y.L. McHall, 1993: Energetics Constraint for Linear Disturbances Development, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 273-286.  doi: 10.1007/BF02658133
    [5] Liu Ruizhi, 1986: A NUMERICAL EXPERIMENT OF CYCLOGENESIS AND THE DEVELOPMENT OF DISTURBANCES, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 499-504.  doi: 10.1007/BF02657939
    [6] Zhang Pei, Ni Yunqi, 1991: The Effect of Topographic Forcing on the Formation and Maintenance of Blocking, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 317-326.  doi: 10.1007/BF02919614
    [7] Lu Peisheng, 1995: Evolution of Asian Summer Monsoon and the Slowly Varying Disturbances, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 311-318.  doi: 10.1007/BF02656979
    [8] Li Shuanglin, Ji Liren, Lin Wantao, 2001: On the Formation and Maintenance of the Persistent Anomalies of Summertime Circulation over the Ural Mountains, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 819-830.
    [9] Zhu Weijun, Sun Zhaobo, 1999: Influence of ENSO Event on the Maintenance of Pacific Storm Track in the Northern Winter, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 630-640.  doi: 10.1007/s00376-999-0037-9
    [10] Xu Jianjun, Wu Guoxiong, 1999: Dynamic Features and Maintenance Mechanism of Asian Summer Monsoon Subsystem, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 523-536.  doi: 10.1007/s00376-999-0028-x
    [11] Xia Daqing, Zheng Liangjie, 1986: NUMERICAL SIMULATION OF THE GENERATION OF MESOSCALE CONVECTTVE SYSTEMS IN LARGE-SCALE ENVIRONMENT, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 360-370.  doi: 10.1007/BF02678656
    [12] Zuohao Cao, G.W.K. Moore, 1998: A Diagnostic Study of Moist Potential Vorticity Generation in an Extratropical Cyclone, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 152-166.  doi: 10.1007/s00376-998-0036-2
    [13] 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
    [14] Xingyan ZHOU, Riyu LU, Guanghua CHEN, Liang WU, 2018: Interannual Variations in Synoptic-Scale Disturbances over the Western North Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 507-517.  doi: 10.1007/s00376-017-7143-x
    [15] Lu Peisheng, 1993: The Propagation of Disturbances Excited by Low-Frequency Oscillations in the Tropics, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 287-295.  doi: 10.1007/BF02658134
    [16] Arona DIEDHIOU, Luiz A. T. MACHADO, Henri LAURENT, 2010: Mean Kinematic Characteristics of Synoptic Easterly Disturbances over the Atlantic, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 483-499.  doi: 10.1007/s00376-009-9092-5
    [17] Zhao Shengju, Zhou Chaodong, 1986: MODELS FOR MEDIUM- AND LONG-RANGE FORECAST-ING OF THE AMOUNT OF MIGRATION OF FIRST-GENERATION MOTHS INTO THE OUTBREAKING AREA OF THE SECOND- GENERATION ARMYWORM, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 379-384.  doi: 10.1007/BF02678658
    [18] GAO Yanhong, CHEN Yuchun, Lü Shihua, 2004: Numerical Simulation of the Critical Scale of Oasis Maintenance and Development in the Arid Regions of Northwest China, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 113-124.  doi: 10.1007/BF02915685
    [19] Li Shuanglin, Ji Liren, Lin Wantao, Ni Yunqi, 2001: The Maintenance of the Blocking over the Ural Mountains during the Second Meiyu Period in the Summer of 1998, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 87-105.  doi: 10.1007/s00376-001-0006-4
    [20] JIANG Jianying, NI Yunqi, 2004: Diagnostic Study on the Structural Characteristics of a Typical Mei-yu Front System and Its Maintenance Mechanism, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 802-813.  doi: 10.1007/BF02916376

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Manuscript History

Manuscript received: 10 January 1984
Manuscript revised: 10 January 1984
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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ON THE GENERATION AND MAINTENANCE OF ATMOSPHERIC DISTURBANCES

  • 1. InstituteofAtmosphericPhysics,AcademiaSinica,Beijing,InstituteofAtmosphericPhysics,AcademiaSinica,Beijing,InstituteofAtmosphericPhysics,AcademiaSinica,Beijing,InstituteofAtmosphericPhysics,AcademiaSinica,Beijing

Abstract: Blocking is one of the intensive atmospheric disturbances which can maintain for a long time. In this paprer we investigate the general conditions favorable for the generation and maintenance of the intensive disturbances. First, the evolutional process of disturbances superimposed on a jet-like zonal flow is studied by using the wave-packet representation and the WKBJ method. Second, the mechanism for generation and maintenance of disturbances is investigated by using the nonlinear equations and the general physical laws. Finally, some numerical experiments are given for illustration, showing the rapid absorption of disturbances by the jet-like zonal flow in one case and the maintenance of disturbances for a long time in the other case.

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