Abstract. Aromatic hydrocarbons, including benzene, toluene, and xylenes, play an
important role in atmospheric chemistry, but the associated chemical mechanisms
are complex and uncertain. Sparing representation of this chemistry in models is
needed for computational tractability. Here, we develop a new compact mechanism
for aromatic chemistry (GC13) that captures current knowledge from laboratory
and computational studies with only 17 unique species and 44 reactions. We
compare GC13 to six other currently used mechanisms of varying complexity in
box model simulations of environmental chamber data and diurnal boundary layer
chemistry, and show that GC13 provides results consistent with or better than
more complex mechanisms for oxygenated products (alcohols, carbonyls,
dicarbonyls), ozone, and hydrogen oxide (HOx≡OH+HO2)
radicals. Specifically, GC13 features increased radical recycling and
increased ozone destruction from phenoxy–phenylperoxy radical cycling relative
to other mechanisms. We implement GC13 into the GEOS-Chem global chemical
transport model and find higher glyoxal yields and net ozone loss from
aromatic chemistry compared with other mechanisms. Aromatic oxidation in the
model contributes 23 %, 5 %, and 8 % of global
glyoxal, methylglyoxal, and formic acid production, respectively, and has mixed
effects on formaldehyde. It drives small decreases in global tropospheric OH
(−2.2 %), NOx (≡NO+NO2; −3.7 %), and
ozone (−0.8 %), but a large increase in NO3 (+22 %) from phenoxy–phenylperoxy radical cycling. Regional effects in
polluted environments can be substantially larger, especially from the photolysis
of carbonyls produced by aromatic oxidation, which drives large wintertime
increases in OH and ozone concentrations.