Classical London smog is called reducing smog because it forms under cool, humid conditions from coal smoke, sulfur dioxide, and reducing particulate material. Fog droplets promote sulfur chemistry and trap soot near the ground during temperature inversions. Los Angeles or photochemical smog is instead strongly oxidising because sunlight generates ozone, peroxyacyl nitrates, and other photochemical oxidants. Atmospheric inversions can trap contaminants near the surface, while wind, turbulence, precipitation, and chemical transformation determine their eventual distribution and removal. At orga
Ref:
Campbell Biology, Urry et al., 12th Ed., Unit 8 Ecology