In the summer, nitrogen dioxide and methane react with chlorine monoxide and chlorine atoms which results in a shrinkage of chlorine and hence prevents ozone layer depletion.
ClO(g)⋅+NO2(g)⟶ClO(X)NO2(g)
Cl(g)+CH4(g)→CH3(g)+HCl(g)
During winter, special types of clouds are formed over the Antarctic region. These clouds provide the surface for the hydrolysis of chlorine nitrate to form hypochlorous acid.
ClONO2(g)+H2O(g)→HOCl(g)+HNO3(g)(Y)(Z)
So, X=ClONO2,Y=HOCl,Z=HNO3