High ozone concentrations have been a major pollution problem in the Mexico
City basin for at least 10 years, exceeding 110 ppbv (Mexican standard) mo
re than 300 days per year. Aircraft observations obtained during February 1
991 showed for the first time that vertical profiles of aerosol particles a
nd ozone presented peak concentrations close to the top of the mixed layer.
We hypothesize that the interplay between aerosol particles, solar radiati
on and photochemical processes is the key to the development of the elevate
d ozone peak. This peak is reproduced when a layer of highly absorbing part
icles, representative of Mexico City aerosols, is included in a 1-D turbule
nt transport and chemistry model of the boundary layer. The results suggest
that the presence of large concentrations of absorbing particles within th
e mixed layer is likely inhibiting ozone formation that would otherwise rea
ch even higher levels. (C) 2000 Elsevier Science Ltd. All rights reserved.