On the Modeling of Thermal Mechanism of Vortex Generation in the Lower Atmosphere

Abstract

Energy dissipation in the atmosphere layer near the Earth surface is associated with diffusive and convective processes, which are determined by differential equations of the second order. Self-consistency in hydrodynamic equations systems is a particularly difficult mathematical problem. Therefore, there is a method of using simplifying assumptions in order to receive an image of atmospheric mass motion. Namely, during any laminar motion in the sea or atmosphere there may generate a vortex that will cause a local perturbance.