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Scale Analysis and Physical Mechanism of Semi-Geostrophic Adaptation in the Tropical Atmosphere

Liu Shikuo and Sun Feng (Department of Geophysics, Peking University, Beijing 100871)  
The scale analysis on planetary scale motion in the tropical atmosphere shows that the equilibrium between the pressure gradient force and Coriolis force in the meridional direction is easily established, which is known as the zonally semi-geostrophic motion The semi-geostrophic adaptation process in which the inertial gravity waves play an important part is relatively quick The evolution process after the semi-geostrophic adaptation process is slow and controlled by the Kelvin waves and long Rossby waves
【Fund】: 国家自然科学基金!49775260
【CateGory Index】: P444
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