(d)
Classical or London type smog is formed by the combination of soot particles with oxides of sulphur while climate is cool and humid. Due to presence of soot and oxides of sulphur, it is reducing in nature.
Photochemical smog or Los Angeles smog is obtained from nitrogen oxides when climate is warm, dry and sunny. Due to presence of $O_{3}\ and\ NO_{2}$ (strong oxidising agents), it is oxidising in nature.
CO does not play any role in the formation of photochemical smog