Water in a tank spins fast, and a column appears that lives long even though everything around it is churning. This column is a vortex, and it doesn't disappear because waves feed it.
Waves are born at the tank walls and travel inward, like ripples across a pond. When a wave enters the vortex, it gives up its energy. This happens in a special place where the wave's speed matches the rotation speed of the water. There, the wave sort of melts, and its energy transfers to the vortex.
Now it's clear why ocean eddies and atmospheric cyclones live so long. They, too, can drink waves that come from far away.
The characteristic wavenumber $k_f$ in the experiments is on the order of 1 cm⁻¹, meaning a wavelength of about a centimeter, while the vortex has a radius of about 40 cm. The vortex lives for tens of its own rotation periods, even though it is fed by waves that are fully absorbed within fractions of a second.