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The Phenomena of Bifurcation and Catastrophe of Large-Scale Horizontal Motion in the Atmosphere under the Effect of Rossby Parameter

The Phenomena of Bifurcation and Catastrophe of Large-Scale Horizontal Motion in the Atmosphere under the Effect of Rossby Parameter

作     者:万军 杨芳林 

作者机构:Chendu Meteorological Institute. Chendu 610041 Institute of Atmospheric PhysicsAcademia SincaBeijinghe stability question of large-scale horizontal motion in the atmosphere under the effect of Rossby parameter is discussed in this paper by using the qualitative analysis theory of ordinary differential equations. The following aspects are reviewed: The stability of large-scale horizontal motion in the atmosphere accords with the common inertial stability criterion when the effect of Rossby parameter is not considered (Yang 1983) and that on the other hand the motion will bifurcate two times with the variation of absolute vorticity of basic Zephyr flow at the initial position under the effect of Rossby parameter. Furthermore in the inertial stable region if the effect of geostrophic deviation at the initial position is considered the motion will not only bifurcate but also generate a catastrophe. 

出 版 物:《Advances in Atmospheric Sciences》 (大气科学进展(英文版))

年 卷 期:1990年第7卷第4期

页      面:409-422页

核心收录:

学科分类:07[理学] 070601[理学-气象学] 0706[理学-大气科学] 

主  题:The Phenomena of Bifurcation and Catastrophe of Large Scale Horizontal Motion in the Atmosphere under the Effect of Rossby Parameter 

摘      要:The stability question of large-scale horizontal motion in the atmosphere under the effect of Rossby parameter is discussed in this paper by using the qualitative analysis theory of ordinary differential equations. The following aspects are reviewed: The stability of large-scale horizontal motion in the atmosphere accords with the common inertial stability criterion when the effect of Rossby parameter is not considered (Yang, 1983), and that, on the other hand, the motion will bifurcate two times with the variation of absolute vorticity of basic Zephyr flow at the initial position under the effect of Rossby parameter. Furthermore, in the inertial stable region, if the effect of geostrophic deviation at the initial position is considered, the motion will not only bifurcate but also generate a catastrophe.

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