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Volume 1 Issue 1

Jan.  1984

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THE CHARACTERISTICS OF THE FORCED STATIONARY PLANETARY WAVE PROPAGATIONS IN SUMMER NORTHERN HEMISPHERE


doi: 10.1007/BF03187619

  • The three-dimensional propagations of the forced stationary planetary waves in a realistic summer current, in which the vertical and horizontal wind shears are included, are discussed by using the refractive index squared of waves in a spherical coordinate system.The results show that there is no polar wave guide in stationary planetary wave propagations in summer. Thus, stationary planetary waves cannot propagate into the stratosphere. However, there are a wave guide pointing from the subtropics toward middle and high latitudes in the troposphere and another wave guide pointing from the lower troposphere at middle latitudes toward the upper troposphere near 30oN in the forced stationary planetary wave propagations.A linearized, steady-state, quasi-geostrophic 34-level spherical coordinate model with Rayleigh friction and Newtonian cooling, horizontal kinematic thermal diffusivity is used to simulate the wave guides of three-dimensional propagations of stationary planetary waves in summer.
  • [1] LI Qian, Hans-F. GRAF, CUI Xuefeng, 2011: The Role of Stationary and Transient Planetary Waves in the Maintenance of Stratospheric Polar Vortex Regimes in Northern Hemisphere Winter, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 187-194.  doi: 10.1007/s00376-010-9163-7
    [2] Lu Peisheng, 1992: The Structure and Propagation of Stationary Planetary Wave Packet in the Barotropic Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 157-166.  doi: 10.1007/BF02657506
    [3] Chen Wen, Huang Ronghui, 2002: The Propagation and Transport Effect of Planetary Waves in the Northern Hemisphere Winter, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 1113-1126.  doi: 10.1007/s00376-002-0069-x
    [4] Claudia Christine STEPHAN, Yan Ho NG, Nicholas P. KLINGAMAN, 2018: On Northern Hemisphere Wave Patterns Associated with Winter Rainfall Events in China, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 1021-1034.  doi: 10.1007/s00376-018-7267-7
    [5] Yong. L. McHall, 1991: Planetary Stationary Waves in the Atmosphere Part I: Orographic Stationary Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 211-224.  doi: 10.1007/BF02658095
    [6] Yong. L. McHall, 1991: Planetary Stationary Waves in the Atmosphere Part II: Thermal Stationary Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 225-236.  doi: 10.1007/BF02658096
    [7] YUAN Wei, SUN Jianqi, 2009: Enhancement of the Summer North Atlantic Oscillation Influence on Northern Hemisphere Air Temperature, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 1209-1214.  doi: 10.1007/s00376-009-8148-x
    [8] HUANG Gang, LIU Yong, HUANG Ronghui, 2011: The Interannual Variability of Summer Rainfall in the Arid and Semiarid Regions of Northern China and Its Association with the Northern Hemisphere Circumglobal Teleconnection, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 257-268.  doi: 10.1007/s00376-010-9225-x
    [9] Alexey V.ELISEEV, Igor I. MOKHOV, 2003: Amplitude-Phase Characteristics of the Annual Cycle of Surface Air Temperature in the Northern Hemisphere, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 1-16.  doi: 10.1007/BF03342045
    [10] Yong. L. McHall, 1992: Nonlinear Planetary Wave Instability and Blocking, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 173-190.  doi: 10.1007/BF02657508
    [11] 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
    [12] Huang Ronghui, 1985: THE NUMERICAL SIMULATION OF THE THREE-DIMEN-SIONAL TELECONNECTIONS IN THE SUMMER CIRCULA-TION OVER THE NORTHERN HEMISPHERE, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 81-92.  doi: 10.1007/BF03179740
    [13] Ni Yunqi, Bette L. Otto-Bliesner, David D. Houghton, 1988: THE EFFECTS OF TOPOGRAPHY ON THE SUMMER ATMOS-PHERIC ENERGETICS OF THE NORTHERN HEMISPHERE IN A LOW-RESOLUTION GLOBAL SPECTRAL MODEL, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 181-194.  doi: 10.1007/BF02656780
    [14] Guo Shichang, Wei Dingwen, 1988: CHARACTERISTICS OF THE TEMPORAL-SPATIAL VARIA-TION IN ATMOSPHERIC OZONOSPHERE OVER THE NORTHERN HEMISPHERE DURING THE PERIOD OF 1963-1985, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 361-368.  doi: 10.1007/BF02656759
    [15] Zhu Zhengxin, 1985: EQUILIBRIUM STATES OF PLANETARY WAVES FORCED BY TOPOGRAPHY AND PERTURBATION HEATING AND BLOCKING SITUATION, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 359-367.  doi: 10.1007/BF02677252
    [16] Lu Keli, Zhu Yongchun, 1994: Seasonal Variation of Stationary and Low-Frequency Rossby Wave Rays, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 427-435.  doi: 10.1007/BF02658163
    [17] Luo Dehai, 1990: Topographically Forced Rossby Wave Instability and the Development of Blocking in the Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 7, 433-440.  doi: 10.1007/BF03008873
    [18] Ho Nam CHEUNG, ZHOU Wen, Hing Yim MOK, Man Chi WU, Yaping SHAO, 2013: Revisiting the Climatology of Atmospheric Blocking in the Northern Hemisphere, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 397-410.  doi: 10.1007/s00376-012-2006-y
    [19] 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
    [20] Li Guoqing, Robin Kung, Richard L. Pfeffer, 1993: Some Effects of Rotation Rate on Planetary-Scale Wave Flows, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 296-306.  doi: 10.1007/BF02658135

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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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THE CHARACTERISTICS OF THE FORCED STATIONARY PLANETARY WAVE PROPAGATIONS IN SUMMER NORTHERN HEMISPHERE

  • 1. InstituteofAtmosphericPhysics,AcademiaSinica,Beijing

Abstract: The three-dimensional propagations of the forced stationary planetary waves in a realistic summer current, in which the vertical and horizontal wind shears are included, are discussed by using the refractive index squared of waves in a spherical coordinate system.The results show that there is no polar wave guide in stationary planetary wave propagations in summer. Thus, stationary planetary waves cannot propagate into the stratosphere. However, there are a wave guide pointing from the subtropics toward middle and high latitudes in the troposphere and another wave guide pointing from the lower troposphere at middle latitudes toward the upper troposphere near 30oN in the forced stationary planetary wave propagations.A linearized, steady-state, quasi-geostrophic 34-level spherical coordinate model with Rayleigh friction and Newtonian cooling, horizontal kinematic thermal diffusivity is used to simulate the wave guides of three-dimensional propagations of stationary planetary waves in summer.

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