The ozone layer is being depleted. During the summer, nitrogen dioxide and methane interacted with chlorine monoxide and chlorine radicle, respectively, to produce chlorine sinks, avoiding ozone depletion.
ClO + NO2 (g) → ClONO2
Cl (g) + CH4→ CH3(g) + HCl (g)
ClONO2 (g) +H2O → HOCl (g) + HNO3
ClONO2 (g) + HCl → Cl2 (g) + HNO3 (g)
When the sunshine returned in the spring, it broke apart clouds, and sunlight photolyzed HOCl and molecular chlorine, forming chlorine radicles: