Photochemical smog, or ground-level ozone, has been the most recalcitr
ant of air pollution problems, but reductions in emissions of sulfur a
nd hydrocarbons may yield unanticipated benefits in air quality. While
sulfate and some organic aerosol particles scatter solar radiation ba
ck into space and can cool Earth's surface, they also change the actin
ic flux of ultraviolet (UV) radiation. Observations and numerical mode
ls show that UV-scattering particles in the boundary layer accelerate
photochemical reactions and smog production, but UV-absorbing aerosols
such as mineral dust and soot inhibit smog production. Results could
have major implications for the control of air pollution.