A stable and cold polar vortex isolates air, allowing the formation of Polar Stratospheric Clouds (PSCs). Reactions on PSCs activate inert chlorine compounds into ozone-depleting forms. The vortex also prevents mixing with ozone-rich air. When the vortex collapses, the isolated, chlorine-activated air mixes with air from lower latitudes, diluting the concentration of activated chlorine. Warmer temperatures also deactivate chlorine. This dispersion and deactivation reduce the rate of ozone depletion.