热带地转适应运动的动力学基础
ON THE DYNAMICAL BASIS OF GEOSTRAPHIC MOTION IN TROPICS
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摘要: 文中讨论了热带斜压大气地转适应过程中的若干动力学约束关系,在不考虑行星位势涡度梯度的前提下给出了三维重力惯性波的频散方程、位势涡度时间不变式。在这基础上指出由于Taylor-Proudman定理成立,运动将趋于水平化。同时指出,在热带纬圈半地转平衡更易出现。地转适应后的运动,一般是水平无辐散的,虽然垂直运动趋于零,但物理场随高度仍然有变化,即是层结的。Abstract: Some conditions of dynamic contract of geostraphic motion in the tropical baroclinic atmosphere are given. The equation of dispassion of gravity-intertia wave and the equation of potential voticity time irrelevance are obtained. It is indicated that motions approach horizontal based on the right of Taylor-proudman theorem in tropics. The motions become horizontal and nondivergence but still are stratificative after geostraphic balance established.