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Abstract
Based on dynamical characteristics of the tropical atmosphere,a mathematical model of low-frequency oscillation (LFO hereinafter) in low-latitudes has been developed.The analysis shows that the distributive features (shear of wind speed) of easterlies and westerlies in low-latitudes,the divergence and convergence of meridional and zonal flow,the vertical structure of diabatic heating and the Coriolis parameter f are the basic factors resulting in the LFO,while quasi-periodical baroclinity development or index cycle of westerly waves in middle-latitudes of the Southern Hemisphere is an external forcing to the LFO in the tropical atmosphere.The resonance on adequate condition makes LFO suddenly enhanced.
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Citation
Xu Xiangde, He Jinhai, Zhu Qiangen. 1990: A DYNAMICAL ANALYSIS OF BASIC FACTORS OF LOW-FREQUENCY OSCILLATION IN THE TROPICAL ATMOSPHERE*. Journal of Meteorological Research, 4(2): 157-167.
Xu Xiangde, He Jinhai, Zhu Qiangen. 1990: A DYNAMICAL ANALYSIS OF BASIC FACTORS OF LOW-FREQUENCY OSCILLATION IN THE TROPICAL ATMOSPHERE*. Journal of Meteorological Research, 4(2): 157-167.
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Xu Xiangde, He Jinhai, Zhu Qiangen. 1990: A DYNAMICAL ANALYSIS OF BASIC FACTORS OF LOW-FREQUENCY OSCILLATION IN THE TROPICAL ATMOSPHERE*. Journal of Meteorological Research, 4(2): 157-167.
Xu Xiangde, He Jinhai, Zhu Qiangen. 1990: A DYNAMICAL ANALYSIS OF BASIC FACTORS OF LOW-FREQUENCY OSCILLATION IN THE TROPICAL ATMOSPHERE*. Journal of Meteorological Research, 4(2): 157-167.
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