Temporal variation of oxides of sulphur and nitrogen in ambient air in eastern Canada: 1979-1994

The temporal variation of daily ambient concentrations of particulate SO 2 4 -, NO 3 - , NH 4 + and gaseous SO 2 and HNO 3 , and total-NO 3 (i.e. HNO 3 + NO 3 ) in eastern Canada was studied by fitting (using the maximum likelihood statistical technique) a temporal model that included long-term tren...

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Veröffentlicht in:Tellus. Series B, Chemical and physical meteorology Chemical and physical meteorology, 1997-01, Vol.49 (3), p.270-291
1. Verfasser: Sirois, Alain
Format: Artikel
Sprache:eng
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Zusammenfassung:The temporal variation of daily ambient concentrations of particulate SO 2 4 -, NO 3 - , NH 4 + and gaseous SO 2 and HNO 3 , and total-NO 3 (i.e. HNO 3 + NO 3 ) in eastern Canada was studied by fitting (using the maximum likelihood statistical technique) a temporal model that included long-term trend, long-term cycles, seasonal cycles and an auto-regressive model. The technique allowed for missing data and used kernel smoothing and spectral analysis to facilitate the selection of the right model. It was first found that the long-term trends were neither linear nor monotonic. Between the beginning of the 80s and 90s, SO 2 ambient air concentration decreased by 21 to 43% at 5 of the 8 sites. During the same period HNO 3 and total-NO 3 concentrations increased at 7 of the 8 sites. For the other compounds, no systematic variations were found for that period and any overall increases or decreases were small. Long-term cycles were found for 70% of the time-series but their amplitudes were small and they represented only a small fraction of the total variance for each time-series. Seasonal cycles with large amplitudes were found only for SO 2 . For the other compounds, statistically significant seasonal cycles were obtained but they had small amplitudes. Auto-regressive models of order 2 were necessary for most of the time-series. For some SO 2 and NO 3 - time-series, auto-regressive models of order 1 were sufficient. For the other compounds, auto-regressive models of order 3 were necessary for some of the time-series. These results indicate that the air masses that arrived at the sites were less homogeneous in the case of SO 2 and NO 3 - than for the other compounds.
ISSN:0280-6509
1600-0889
DOI:10.3402/tellusb.v49i3.15967