A new method is given for transforming the initial nonlinear equations for the two-dimensional stationary case of altitude stratification in the atmosphere, where a slight simplification in the equation of continuity enables one to derive interesting particular cases where the flow treatment amounts exactly to solving a linear equation for the streamline function. A study is made to see how well one can incorporate the altitude profiles for the stability and velocity. The approach is compared with previous ones.
Department of Physics of Atmosphere, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
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