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STUDY OF PHYSICAL MECHANISM FOR ACTIVE AND BREAK PHASES OF SOUTH ASIAN MONSOON

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  • Using a low-order spectral model derived from the equatorial equilibrium model, possible physical mechanisms are interpreted by the theory of multiple equilibria states for the active and break phases of the South Asian Monsoon, with consideration of the effects of heating by cumulus heating and cooling by radiation. The result shows that the South Asian Monsoon is active when the cumulus convection intensifies (or the radiation cooling weakens). the monsoon breaks when the convection weakens (or the cooling intensifies). It is consistent with the hypothesis of cloud-radiation by Krishnamurti et al.
  • [1] Coswami B N. 1983. Theoretical study of multiple equilibria in simple axisymmetric tropical circulation. Tellus. 35: 119-135.
    [2] Krishnamurti T N. Bhalme H H. 1976. Oscillations of a monsoon system. Part I:Observational aspects. J. Atmos. Sci,33:1937-1954.
    [3] Zhao Jingxia. Zhu Baozhen, 1989. Sensitivity of the multiple equilibria to governing system. mode chosen and parameter Adv. in.Atmos. Sci,6: 33-43
    [4] Zebiak S E. 1986. Atmospheric convergence feedback in a simple model for El Nmo, Mon. Wea. Rev,114:1263-1271.
    [5] Zhu Baozhen. Zhau Jingxia, 1989. Multiple flow equilibria in tropical circulation monsoon.,Adv. in Atrnos. Sci.4:375-384.

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Wu Hong, Wang Yongzhong, Xia Youlong. STUDY OF PHYSICAL MECHANISM FOR ACTIVE AND BREAK PHASES OF SOUTH ASIAN MONSOON [J]. Journal of Tropical Meteorology, 1998, 4(2): 122-130.
Wu Hong, Wang Yongzhong, Xia Youlong. STUDY OF PHYSICAL MECHANISM FOR ACTIVE AND BREAK PHASES OF SOUTH ASIAN MONSOON [J]. Journal of Tropical Meteorology, 1998, 4(2): 122-130.
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Manuscript History

Manuscript received: 10 October 1995
Manuscript revised: 28 July 2011
通讯作者: 陈斌, bchen63@163.com
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STUDY OF PHYSICAL MECHANISM FOR ACTIVE AND BREAK PHASES OF SOUTH ASIAN MONSOON

Abstract: Using a low-order spectral model derived from the equatorial equilibrium model, possible physical mechanisms are interpreted by the theory of multiple equilibria states for the active and break phases of the South Asian Monsoon, with consideration of the effects of heating by cumulus heating and cooling by radiation. The result shows that the South Asian Monsoon is active when the cumulus convection intensifies (or the radiation cooling weakens). the monsoon breaks when the convection weakens (or the cooling intensifies). It is consistent with the hypothesis of cloud-radiation by Krishnamurti et al.

Wu Hong, Wang Yongzhong, Xia Youlong. STUDY OF PHYSICAL MECHANISM FOR ACTIVE AND BREAK PHASES OF SOUTH ASIAN MONSOON [J]. Journal of Tropical Meteorology, 1998, 4(2): 122-130.
Citation: Wu Hong, Wang Yongzhong, Xia Youlong. STUDY OF PHYSICAL MECHANISM FOR ACTIVE AND BREAK PHASES OF SOUTH ASIAN MONSOON [J]. Journal of Tropical Meteorology, 1998, 4(2): 122-130.
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