Research over the past ten years has created a more detailed and coherent v
iew of the relation between O-3 and its major anthropogenic precursors, vol
atile organic compounds (VOC) and oxides of nitrogen (NOx). This article pr
esents a review of insights derived from photochemical models and field mea
surements. The ozone-precursor relationship can be understood in terms of a
fundamental split into a NOx-senstive and VOC-sensitive (or NOx-saturated)
chemical regimes. These regimes are associated with the chemistry of odd h
ydrogen radicals and appear in different forms in studies of urbanized regi
ons, power plant plumes and the remote troposphere. Factors that affect the
split into NO, sensitive and VOC-sensitive chemistry include: VOC/NOx rati
os, VOC reactivity, biogenic hydrocarbons, photochemical aging, and rates o
f meteorological dispersion. Analyses of ozone-NOx-VOC sensitivity from 3D
photochemical models show a consistent pattern, but predictions for the imp
act of reduced NOx and VOC in indivdual locations are often very uncertain.
This uncertainty can be identified by comparing predictions from different
model scenarios that reflect uncertainties in meteorology, anthropogenic a
nd biogenic emissions. Several observation-based approaches have been propo
sed that seek to evaluate ozone-NOx-VOC sensitivity directly from ambient m
easurements (including ambient VOC, reactive nitrogen, and peroxides). Obse
rvation-based approaches have also been used to evaluate emission rates, oz
one production efficiency, and removal rates of chemically active species.
Use of these methods in combination with models can significantly reduce th
e uncertainty associated with model predictions. (C) 1999 Elsevier Science
Ltd. All rights reserved.