“…The vertical velocity in the vortex, required to create an observed disturbance, is in the order of 10-20 m/s. It qualitatively corresponds to the typical velocity obtained during the collapse of the hot cavern in the late stages of the current pulse [27]. The vortex intensity does not depend on the local flow velocity, since the momentum coefficient is rather high, C µ > 1, and the pulse duration is in the order of the convection time, τ = D/U 0 ∼ 90 µs, at U 0 = 80 m/s.…”