Near centers of low or high pressure, the wind rotates along curved paths. A good approximation to the real wind that has that behavior is the gradient wind. This model consists of considering a balance between the forces of the pressure gradient, Coriolis and the force centrifugal a) Deduce the gradient wind speed. In a tornado, the spinning wind can reach 30 m/s at a distance 300 m from the center. Under these conditions, in the gradient wind it is possible to neglect the Coriolis term. This model is called wind cyclostrophic and can describe a tornado in a mature state of development. However, it is a slightly imprecise model due to the great acceleration

b) Deduce the speed of the cyclostrophic wind

vertical that is experienced in tornadoes, where the balance is not met hydrostatic.