Non-linear evolution of a barotropically unstable circumpolar vortex, which is an idealization of the polar night jet in the stratosphere, is investigated by numerical time-integrations of a full non-linear vorticity equation over wide ranges of several external parameters of the jet. Some non-linear features which cannot be expected in the linear stability analysis are obtained in the time-integrations.Two types of stabilization processes are found in diagnosis of the non-linear evolution with daily maps of the absolute vorticity field: The negative gradient of absolute vorticity on the equator-ward side of the jet disappears owing to the vorticity mixing by the growth of thin vortex filaments in middle latitudes, while the negative gradient on the poleward side of the jet disappears owing to the equator-ward displacement of the polar fluid with low absolute vorticity.Decrease of dominant wavenumber is observed in the non-linear phase of the evolution for wide parameter ranges. An eastward-propagating wave of zonal wavenumber 2 becomes dominant after the stabilization of the circumpolar vortex that is unstable in middle latitudes, even if the exponential growth rate of this wave is not the largest in the linear stability analysis.