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Seasonal influences on surface ozone variability in continental South Africa and implications for air quality.

Authors :
Laban TL
van Zyl PG
Beukes JP
Vakkari V
Jaars K
Borduas-Dedekind N
Josipovic M
Thompson AM
Kulmala M
Laakso L
Source :
Atmospheric chemistry and physics [Atmos Chem Phys] 2018 Oct; Vol. 18 (20), pp. 15491-15514. Date of Electronic Publication: 2018 Oct 29.
Publication Year :
2018

Abstract

Although elevated surface ozone (O <subscript>3</subscript> ) concentrations are observed in many areas within southern Africa, few studies have investigated the regional atmospheric chemistry and dominant atmospheric processes driving surface O <subscript>3</subscript> formation in this region. Therefore, an assessment of comprehensive continuous surface O <subscript>3</subscript> measurements performed at four sites in continental South Africa was conducted. The regional O <subscript>3</subscript> problem was evident, with O <subscript>3</subscript> concentrations regularly exceeding the South African air quality standard limit, while O <subscript>3</subscript> levels were higher compared to other background sites in the Southern Hemisphere. The temporal O <subscript>3</subscript> patterns observed at the four sites resembled typical trends for O <subscript>3</subscript> in continental South Africa, with O <subscript>3</subscript> concentrations peaking in late winter and early spring. Increased O <subscript>3</subscript> concentrations in winter were indicative of increased emissions of O <subscript>3</subscript> precursors from household combustion and other low-level sources, while a spring maximum observed at all the sites was attributed to increased regional biomass burning. Source area maps of O <subscript>3</subscript> and CO indicated significantly higher O <subscript>3</subscript> and CO concentrations associated with air masses passing over a region with increased seasonal open biomass burning, which indicated CO associated with open biomass burning as a major source of O <subscript>3</subscript> in continental South Africa. A strong correlation between O <subscript>3</subscript> on CO was observed, while O <subscript>3</subscript> levels remained relatively constant or decreased with increasing NO <subscript> x </subscript> , which supports a VOC-limited regime. The instantaneous production rate of O <subscript>3</subscript> calculated at Welgegund indicated that ~ 40 % of O <subscript>3</subscript> production occurred in the VOC-limited regime. The relationship between O <subscript>3</subscript> and precursor species suggests that continental South Africa can be considered VOC limited, which can be attributed to high anthropogenic emissions of NO <subscript> x </subscript> in the interior of South Africa. The study indicated that the most effective emission control strategy to reduce O <subscript>3</subscript> levels in continental South Africa should be CO and VOC reduction, mainly associated with household combustion and regional open biomass burning.<br />Competing Interests: Competing interests. The authors declare that they have no conflict of interest.

Details

Language :
English
ISSN :
1680-7316
Volume :
18
Issue :
20
Database :
MEDLINE
Journal :
Atmospheric chemistry and physics
Publication Type :
Academic Journal
Accession number :
32678379
Full Text :
https://doi.org/10.5194/acp-18-15491-2018