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Volume 8 Issue 2

Mar.  1991

Article Contents

Planetary Stationary Waves in the Atmosphere Part II: Thermal Stationary Waves


doi: 10.1007/BF02658096

  • The contribution of thermal forcing to the planetary stationary waves will be studied also by assuming that heat balance in stationary waves over zonally asymmetric thermal forcing must be maintained over a long time period. Us-ing the same model of geostrophic waves introduced in Part I, we may explain successfully the observed and simulated responses to the thermal forcing in the atmosphere, such as the wave 1 structure at high levels of middle latitudes, the seasonal changes of the stationary waves in the Northern Hemisphere, the opposite phase distributions of stationary waves at high and low levels of the subtropical regions in both hemispheres and so on.
  • [1] 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
    [2] 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
    [3] Y. L. McHall, 1993: Large Scale Perturbations in Extratropical Atmosphere-Part II: On Geostrophic Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 181-192.  doi: 10.1007/BF02919140
    [4] 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
    [5] Yong L. McHall, 1993: Group Velocity of Anisotropic Waves-Part II: Conservative Properties, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 407-414.  doi: 10.1007/BF02656965
    [6] Huang Ronghui, 1984: THE CHARACTERISTICS OF THE FORCED STATIONARY PLANETARY WAVE PROPAGATIONS IN SUMMER NORTHERN HEMISPHERE, ADVANCES IN ATMOSPHERIC SCIENCES, 1, 84-104.  doi: 10.1007/BF03187619
    [7] Y. L. McHall, 1993: Large Scale Perturbations in Extratropical Atmosphere-Part I: On Rossby Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 169-180.  doi: 10.1007/BF02919139
    [8] Chen Zhongming, Liu Fuming, Li Xiaoping, Tao Jie, 1994: Oscillatory Rossby Solitary Waves in the Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 65-73.  doi: 10.1007/BF02656995
    [9] Ji Zhengang, Chao Jiping, 1986: ON THE INFLUENCES OF LARGE-SCALE INHOMOGENEITY OF SEA TEMPERATURE UPON THE OCEANIC WAVES IN THE TROPICAL REGIONS PART II: LINEAR NUMERICAL EXPERIMENTS, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 238-244.  doi: 10.1007/BF02682557
    [10] 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
    [11] 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
    [12] Jiang Guorong, 1996: CISK-related Rossby Waves in the Tropical Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 13, 115-123.  doi: 10.1007/BF02657032
    [13] 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
    [14] Yong L. McHall, 1993: Group Velocity of Anisotropic Waves-Part I: Mathematical Expression, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 393-406.  doi: 10.1007/BF02656964
    [15] Luo Dehai, Li Jianping, 2000: Barotropic Interaction between Planetary- and Synoptic-Scale Waves during the Life Cycles of Blockings, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 649-670.  doi: 10.1007/s00376-000-0026-5
    [16] 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
    [17] Li Guitong, Li Chongyin, 1998: Activities of Low-Frequency Waves in the Tropical Atmosphere and ENSO, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 193-203.  doi: 10.1007/s00376-998-0039-z
    [18] 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
    [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] YANG Peicai, WANG Geli, BIAN Jianchun, ZHOU Xiuji, 2010: The Prediction of Non-stationary Climate Series Based on Empirical Mode Decomposition, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 845-854.  doi: 10.1007/s00376-009-9128-x

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Manuscript History

Manuscript received: 10 March 1991
Manuscript revised: 10 March 1991
通讯作者: 陈斌, bchen63@163.com
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Planetary Stationary Waves in the Atmosphere Part II: Thermal Stationary Waves

  • 1. Department of Meteorology, University of Edinburgh, EH9 3JZ, U. K.

Abstract: The contribution of thermal forcing to the planetary stationary waves will be studied also by assuming that heat balance in stationary waves over zonally asymmetric thermal forcing must be maintained over a long time period. Us-ing the same model of geostrophic waves introduced in Part I, we may explain successfully the observed and simulated responses to the thermal forcing in the atmosphere, such as the wave 1 structure at high levels of middle latitudes, the seasonal changes of the stationary waves in the Northern Hemisphere, the opposite phase distributions of stationary waves at high and low levels of the subtropical regions in both hemispheres and so on.

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