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Statistical analysis of factors driving surface ozone variability over continental South Africa

dc.contributor.authorLabana, Tracey Leah
dc.contributor.authorVan Zyl, Pieter Gideon
dc.contributor.authorBeukes, Johan Paul
dc.contributor.authorSantana, Leonard
dc.contributor.authorJosipovic, Miroslav
dc.contributor.researchID10092390 - Beukes, Johan Paul
dc.contributor.researchID22648143 - Josipovic, Miroslav
dc.contributor.researchID10710361 - Van Zyl, Pieter Gideon
dc.contributor.researchID23327278 - Laban, Tracey Leah
dc.contributor.researchID11803371 - Santana, Leonard
dc.date.accessioned2020-07-14T08:45:56Z
dc.date.available2020-07-14T08:45:56Z
dc.date.issued2020
dc.description.abstractStatistical relationships between surface ozone (O3) concentration, precursor species and meteorological conditions in continental South Africa were examined from data obtained from measurement stations in north-eastern South Africa. Three multivariate statistical methods were applied in the investigation, i.e. multiple linear regression (MLR), principal component analysis (PCA) and -regression (PCR), and generalised additive model (GAM) analysis. The daily maximum 8-h moving average O3 concentrations were considered in these statistical models (dependent variable). MLR models indicated that meteorology and precursor species concentrations are able to explain ~50% of the variability in daily maximum O3 levels. MLR analysis revealed that atmospheric carbon monoxide (CO), temperature and relative humidity were the strongest factors affecting the daily O3 variability. In summer, daily O3 variances were mostly associated with relative humidity, while winter O3 levels were mostly linked to temperature and CO. PCA indicated that CO, temperature and relative humidity were not strongly collinear. GAM also identified CO, temperature and relative humidity as the strongest factors affecting the daily variation of O3. Partial residual plots found that temperature, radiation and nitrogen oxides most likely have a non-linear relationship with O3,while the relationship with relative humidity and CO is probably linear. An inter-comparison between O3 levels modelled with the three statistical models compared to measured O3 concentrations showed that the GAM model offered a slight improvement over the MLR model. These findings emphasise the critical role of regional-scale O3 precursors coupled with meteorological conditions in daily variances of O3 levels in continental South Africaen_US
dc.identifier.citationLaban, T.L. et al. 2020. Statistical analysis of factors driving surface ozone variability over continental South Africa. Journal of integrative environmental sciences, 17(3):1-28. [https://doi.org/10.1080/1943815X.2020.1768550]en_US
dc.identifier.issn1943-815X
dc.identifier.issn1943-8168 (Online)
dc.identifier.urihttp://hdl.handle.net/10394/35091
dc.identifier.urihttps://www.tandfonline.com/doi/full/10.1080/1943815X.2020.1768550
dc.identifier.urihttps://doi.org/10.1080/1943815X.2020.1768550
dc.language.isoenen_US
dc.publisherTaylor & Francisen_US
dc.subjectTropospheric ozone (O3)en_US
dc.subjectMultiple linear regressionen_US
dc.subjectPrincipal component analysisen_US
dc.subjectGeneralized additive modelsen_US
dc.subjectWelgegunden_US
dc.titleStatistical analysis of factors driving surface ozone variability over continental South Africaen_US
dc.typeArticleen_US

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