Solar Ultraviolet Radiation in Pretoria and Its Relations to Aerosols and Tropospheric Ozone during the Biomass Burning Season

Biomass burning has an impact on atmospheric composition as well as human health and wellbeing. In South Africa, the biomass burning season extends from July to October and affects the aerosol loading and tropospheric ozone concentrations which in turn impact solar ultraviolet radiation (UVR) levels...

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Main Authors: D. Jean du Preez, Hassan Bencherif, Thierry Portafaix, Kévin Lamy, Caradee Yael Wright
Format: Article
Language:English
Published: MDPI AG 2021-01-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/12/2/132
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author D. Jean du Preez
Hassan Bencherif
Thierry Portafaix
Kévin Lamy
Caradee Yael Wright
author_facet D. Jean du Preez
Hassan Bencherif
Thierry Portafaix
Kévin Lamy
Caradee Yael Wright
author_sort D. Jean du Preez
collection DOAJ
description Biomass burning has an impact on atmospheric composition as well as human health and wellbeing. In South Africa, the biomass burning season extends from July to October and affects the aerosol loading and tropospheric ozone concentrations which in turn impact solar ultraviolet radiation (UVR) levels at the surface. Using ground-based observations of aerosols, tropospheric ozone and solar UVR (as well as modelled solar UVR) we investigated the impact of aerosols and tropospheric ozone on solar UVR in August, September, and October over Pretoria. Aerosol optical depth (AOD) and tropospheric ozone reached a peak between September and October each year. On clear-sky days, the average relative difference between the modelled and observed solar Ultraviolet Index (UVI) levels (a standard indicator of surface UVR) at solar noon was 7%. Using modelled UVR—which included and excluded the effects of aerosols and tropospheric ozone from biomass burning—aerosols had a larger radiative effect compared to tropospheric ozone on UVI levels during the biomass burning season. Excluding only aerosols resulted in a 10% difference between the modelled and observed UVI, while excluding only tropospheric ozone resulted in a difference of −2%. Further understanding of the radiative effect of aerosols and trace gases, particularly in regions that are affected by emissions from biomass burning, is considered important for future research.
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spelling doaj.art-51fbbed87c43422c8e4095cea5cb42672023-12-03T14:01:39ZengMDPI AGAtmosphere2073-44332021-01-0112213210.3390/atmos12020132Solar Ultraviolet Radiation in Pretoria and Its Relations to Aerosols and Tropospheric Ozone during the Biomass Burning SeasonD. Jean du Preez0Hassan Bencherif1Thierry Portafaix2Kévin Lamy3Caradee Yael Wright4LACy, (UMR 8105, CNRS, Université de La Réunion, Méteo-France), 97744 Saint-Denis de La Réunion, FranceLACy, (UMR 8105, CNRS, Université de La Réunion, Méteo-France), 97744 Saint-Denis de La Réunion, FranceLACy, (UMR 8105, CNRS, Université de La Réunion, Méteo-France), 97744 Saint-Denis de La Réunion, FranceLACy, (UMR 8105, CNRS, Université de La Réunion, Méteo-France), 97744 Saint-Denis de La Réunion, FranceDepartment of Geography, Geoinformatics and Meteorology, University of Pretoria, Pretoria 0002, South AfricaBiomass burning has an impact on atmospheric composition as well as human health and wellbeing. In South Africa, the biomass burning season extends from July to October and affects the aerosol loading and tropospheric ozone concentrations which in turn impact solar ultraviolet radiation (UVR) levels at the surface. Using ground-based observations of aerosols, tropospheric ozone and solar UVR (as well as modelled solar UVR) we investigated the impact of aerosols and tropospheric ozone on solar UVR in August, September, and October over Pretoria. Aerosol optical depth (AOD) and tropospheric ozone reached a peak between September and October each year. On clear-sky days, the average relative difference between the modelled and observed solar Ultraviolet Index (UVI) levels (a standard indicator of surface UVR) at solar noon was 7%. Using modelled UVR—which included and excluded the effects of aerosols and tropospheric ozone from biomass burning—aerosols had a larger radiative effect compared to tropospheric ozone on UVI levels during the biomass burning season. Excluding only aerosols resulted in a 10% difference between the modelled and observed UVI, while excluding only tropospheric ozone resulted in a difference of −2%. Further understanding of the radiative effect of aerosols and trace gases, particularly in regions that are affected by emissions from biomass burning, is considered important for future research.https://www.mdpi.com/2073-4433/12/2/132aerosol optical depthAfricaair pollutionatmospheric scienceenvironmental healthozone
spellingShingle D. Jean du Preez
Hassan Bencherif
Thierry Portafaix
Kévin Lamy
Caradee Yael Wright
Solar Ultraviolet Radiation in Pretoria and Its Relations to Aerosols and Tropospheric Ozone during the Biomass Burning Season
Atmosphere
aerosol optical depth
Africa
air pollution
atmospheric science
environmental health
ozone
title Solar Ultraviolet Radiation in Pretoria and Its Relations to Aerosols and Tropospheric Ozone during the Biomass Burning Season
title_full Solar Ultraviolet Radiation in Pretoria and Its Relations to Aerosols and Tropospheric Ozone during the Biomass Burning Season
title_fullStr Solar Ultraviolet Radiation in Pretoria and Its Relations to Aerosols and Tropospheric Ozone during the Biomass Burning Season
title_full_unstemmed Solar Ultraviolet Radiation in Pretoria and Its Relations to Aerosols and Tropospheric Ozone during the Biomass Burning Season
title_short Solar Ultraviolet Radiation in Pretoria and Its Relations to Aerosols and Tropospheric Ozone during the Biomass Burning Season
title_sort solar ultraviolet radiation in pretoria and its relations to aerosols and tropospheric ozone during the biomass burning season
topic aerosol optical depth
Africa
air pollution
atmospheric science
environmental health
ozone
url https://www.mdpi.com/2073-4433/12/2/132
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