The mathematical theory of powerful tornadoes in atmospheric air, in which the angular velocity of the rotation of air masses in the vortex ring of the parent cloud that generates the tornado is much greater than the angular velocity of the rotation of the air flow on the Earth’s surface, is constructed. The theory developed is relevant for applications and allows us to calculate the air flow velocity in a tornado as accurately as desired and to determine the geometric funnel-shaped boundary of a tornado.
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