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STRUCTURES AND CONDITIONS OF EXISTENCE FOR A KIND OF ATMOSPHERIC MOTIONS

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  • With the method of phase plane, the P-coordinated equation sets have been derived that include no friction without the introduction of the kdv equation and the structure of atmospheric motions, conditions for existence and movement are studied for all individual solutions. The result shows that a weak high or low pressure system isjointly affected by the atmospheric static stability, latent heating due to condensation and sensible heating for the conditions for existence, state of movement, structural features.
  • [1] Li Guoping, Lu Jinghua, 1996. Some possible solutions of nonlinear internal inertial gravity wave equations in the atmosphere. Advances in Atmos. Sci., 13: 243-252.
    [2] Lu Jinghua, Lei Xiaotu, 1995. Influence of diabatic heating on isolated waves and application in the atmosphere (in Chinese). Acta Meteor. Sin., 6: 539-549.
    [3] Lu Jinghua, Li Guoping, 1994. Influence of stratification stability and wave velocity on the solution to the isolated wave (in Chinese). J. Geophy., 37: (supplementary Ⅱ) 46-55.
    [4] Qiao Jinming, Zhang Yagao, 1994. On Synoptics of the Tibetan Plateau Beijing: China Meteorological Press 120-155.

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Zhu Zhiyu, Lu Jinghua. STRUCTURES AND CONDITIONS OF EXISTENCE FOR A KIND OF ATMOSPHERIC MOTIONS [J]. Journal of Tropical Meteorology, 1999, 5(1): 87-97.
Zhu Zhiyu, Lu Jinghua. STRUCTURES AND CONDITIONS OF EXISTENCE FOR A KIND OF ATMOSPHERIC MOTIONS [J]. Journal of Tropical Meteorology, 1999, 5(1): 87-97.
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Manuscript History

Manuscript received: 01 December 1997
Manuscript revised: 28 May 1998
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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STRUCTURES AND CONDITIONS OF EXISTENCE FOR A KIND OF ATMOSPHERIC MOTIONS

Abstract: With the method of phase plane, the P-coordinated equation sets have been derived that include no friction without the introduction of the kdv equation and the structure of atmospheric motions, conditions for existence and movement are studied for all individual solutions. The result shows that a weak high or low pressure system isjointly affected by the atmospheric static stability, latent heating due to condensation and sensible heating for the conditions for existence, state of movement, structural features.

Zhu Zhiyu, Lu Jinghua. STRUCTURES AND CONDITIONS OF EXISTENCE FOR A KIND OF ATMOSPHERIC MOTIONS [J]. Journal of Tropical Meteorology, 1999, 5(1): 87-97.
Citation: Zhu Zhiyu, Lu Jinghua. STRUCTURES AND CONDITIONS OF EXISTENCE FOR A KIND OF ATMOSPHERIC MOTIONS [J]. Journal of Tropical Meteorology, 1999, 5(1): 87-97.
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