LONG-TERM DAILY MEAN MIXING RATIOS OF O-3, PAN, HNO3, AND PARTICLE NITRATE AT A RURAL LOCATION IN EASTERN CANADA - RELATIONSHIPS AND IMPLIED OZONE PRODUCTION EFFICIENCY
Jw. Bottenheim et A. Sirois, LONG-TERM DAILY MEAN MIXING RATIOS OF O-3, PAN, HNO3, AND PARTICLE NITRATE AT A RURAL LOCATION IN EASTERN CANADA - RELATIONSHIPS AND IMPLIED OZONE PRODUCTION EFFICIENCY, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D2), 1996, pp. 4189-4204
Temporal trends (long term, annual, and daily) for concurrent observat
ions of O-3, PAN, HNO3, and pNO(3)(-) (particle nitrate) are derived.
Correlations between these compounds and the meteorological parameters
temperature and precipitation are outlined using a partial correlatio
n analysis and a principal component analysis. Long-term trends are ob
served for the nitrogen oxides that do not appear to be due to eastern
North American sources. No long-term trend in O-3 is found, and a dec
rease in the efficiency of its production as function of nitrogen oxid
e abundance is indicated which may be caused by a decrease in the leve
ls of hydrocarbons. Annual cycles of O-3 and PAN show similarity with
a spring peak and a summer minimum. These compounds are positively cor
related at all times but especially so in the spring, independent of t
he annual cycle, and it is inferred that a common mechanism drives the
spring maximum. HNO3 and pNO(3)(-) do not show a similar spring maxim
um: HNO3 maximizes in the summer and pNO(3)(-) in the winter. On a day
-to-day basis, PAN and O-3 show almost identical autocorrelation which
is greater than that for HNO3 and pNO(3)(-), probably due to the vari
ance introduced by precipitation scavenging of the latter. HNO3 and te
mperature correlate negative in the winter and positive in the summer
with O-3 reflecting the different production mechanisms of HNO3. Posit
ive correlation between HNO3 and PAN is seen suggesting that part of t
heir variance is due to their common precursor NOx, while the negative
correlation between PAN and temperature is probably reflecting the th
ermal instability of PAN. The results are used to infer the seasonal v
ariation in the O-3 production efficiency as a function of nitrogen ox
ide abundance. A slight negative value is derived for the winter, and
only during the period May to August is O-3 expected to be produced ef
ficiently.