G. Salisbury et al., Production of peroxy radicals at night via reactions of ozone and the nitrate radical in the marine boundary layer, J GEO RES-A, 106(D12), 2001, pp. 12669-12687
In this paper, a substantial set of simultaneous measurements of the sum of
peroxy radicals, [HO2+RO2], NO3, hydrocarbons (HCs), and ozone, taken at M
ace Head on the Atlantic coast of Ireland in spring 1997, is presented. Con
ditions encountered during the experiment ranged from semipolluted air mass
es advected from Britain and continental Europe to clean air masses off the
North and mid-Atlantic, where mixing ratios of pollution tracers approache
d Northern Hemispheric background mixing ratios. Average mixing ratios of p
eroxy radicals varied from 2.5 to 5.5 parts per trillion by volume (pptv) a
t night depending on wind sector, and were observed to decay only very slow
ly from late afternoon to early morning (0.1-0.5 pptv h(-1)). Measurements
of OH and HO2 on two nights using the Fluorescence Assay by Gas Expansion (
FAGE) technique give an upper limit for [OH] of 2.5x10(5) molecules cm(-3)
and an average upper limit [HO2]/[HO2+RO2] ratio of 0.27. A modeling study
of the (1)/e lifetimes of the peroxy radicals, assuming no radical producti
on at night, yielded mean lifetimes of between similar to 8-23 min for HO2
and 3-18 min for CH3O2. Given these lifetimes, it may be concluded that the
peroxy-radical mixing ratios observed could not be maintained without subs
tantial production at night. No significant correlation is observed between
measured [HO2+RO2] and [NO3] under any conditions. Calculation of the reac
tion rates for ozone and NO, with hydrocarbons (HCs) shows that the ozone-i
nitiated oxidation routes of HCs outweighed those of NO3 in the NE, SE and
NW wind sectors. In the SW sector, however, the two mechanisms operated at
similar rates on average, and oxidation by NO3 was the dominant route in th
e westerly sector. The oxidation of alkenes at night by ozone was greater b
y a factor of 4 than that by NO3 over the whole data set. The HC degradatio
n rates from the three "westerly" sectors, where tracer mixing ratios were
relatively low, may be representative of the nighttime oxidative capacity o
f the marine boundary layer throughout the background Northern Hemisphere.
Further calculations using literature values for OH yields and inferred RO2
yields from the ozone-alkene reactions show that peroxy radicals derived f
rom the ozone reactions were likely to make up the major part of the peroxy
-radical signal at night (mean value 66%). However, the NO3 source was of s
imilar magnitude in the middle of the night, when [NO3] was generally at it
s maximum. The estimated total rates of formation of peroxy radicals are mu
ch higher under semipolluted conditions (mean 8.0x10(4) molecules cm(-3) s(
-1) in the SE wind sector) than under cleaner conditions (mean 2.4x10(4) mo
lecules cm(-3) s(-1) in the westerly wind sector). A model study using a ca
mpaign-tailored box model (CTBM) for semipolluted conditions shows that the
major primary sources of OH, HO2, and CH3O2 (the most abundant organic per
oxy radical) were the Criegee biradical intermediates formed in the reactio
ns of ozone with alkenes.