Abstract:
We consider a system of equations that describes the air motion inside tropical cyclones, including consequences of the condensation of water vapor. We examine the system of nonlinear ordinary differential equations on wind trajectories in the plane of radial and vertical variables. We prove the unique solvability of the system of differential equations on a segment suitable for modeling of tropical cyclones.
Keywords:tropical cyclone, air motion, condensation of water vapor, transport equation, a priori estimate, unique solvability.