Optical properties of atmospheric aerosol over Cape Town, Western Cape of South Africa: Role of biomass burning
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| Format: | Artículo científico |
| Language: | en |
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Universidad Nacional Autónoma de México
2021
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| _version_ | 1876426108181676032 |
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| author | Abdulaziz Tunde Yakubu |
| author_facet | Abdulaziz Tunde Yakubu |
| contents | Optical properties of atmospheric aerosol over Cape Town, Western Cape of South Africa: Role of biomass burning Abdulaziz Tunde Yakubu Naven Chetty Biología back trajectory biomass burning fire radiative power Aerosol optical depth The optical characteristics of atmospheric aerosol are vital in the determination of regional climate trends. Biomass burning is typically known to influence aerosol optical characteristics. Following the incessant biomass burning and the recent drop in precipitation over Western Cape, aerosol optical properties with a focus on the impact of biomass burning are studied over Cape Town using data from the Aerosol Robotic Network (AERONET) and the Moderate Resolution Imaging Spectroradiometer (MODIS). In general terms, measurements from both platforms significantly agree on the estimates of aerosol optical depth (AOD) and water vapor content. The mean AOD (0.075 ± 0.022) and the Ångström exponent (0.63 ± 0.19) derived from AERONET demonstrate the dominance of coarse mode aerosol typical of maritime aerosol. Similarly, aerosol particle size distributions display the predominance of coarse mode particles. However, the derived refractive index is more representative of urban-industrial aerosol. Also, estimated back-trajectories show that more than 70% of the aerosol particles over the region originate over the ocean. Atmospheric vapor increases from winter to summer, mainly influenced by air temperature, supersaturation level, and absorbing aerosol. Furthermore, two significant sources accounted for biomass burning related to high AOD values: local biomass burning and regionally transported aged smoke majorly from elsewhere in Sothern Africa. 2021 artículo científico 0187-6236 https://www.redalyc.org/articulo.oa?id=56572302003 https://www.redalyc.org/journal/565/56572302003/ https://www.redalyc.org/journal/565/56572302003/html/ https://www.redalyc.org/journal/565/56572302003/56572302003.epub https://www.redalyc.org/journal/565/56572302003/movil 10.20937/ATM.52811 en http://www.redalyc.org/revista.oa?id=565 Atmósfera application/pdf Universidad Nacional Autónoma de México Atmósfera (México) Num.4 Vol.34 |
| format | Artículo científico |
| id | redalyc_56572302003 |
| institution | Redalyc |
| language | en |
| publishDate | 2021 |
| publisher | Universidad Nacional Autónoma de México |
| spellingShingle | Optical properties of atmospheric aerosol over Cape Town, Western Cape of South Africa: Role of biomass burning Abdulaziz Tunde Yakubu Biología back trajectory biomass burning fire radiative power Aerosol optical depth Optical properties of atmospheric aerosol over Cape Town, Western Cape of South Africa: Role of biomass burning Abdulaziz Tunde Yakubu Naven Chetty Biología back trajectory biomass burning fire radiative power Aerosol optical depth The optical characteristics of atmospheric aerosol are vital in the determination of regional climate trends. Biomass burning is typically known to influence aerosol optical characteristics. Following the incessant biomass burning and the recent drop in precipitation over Western Cape, aerosol optical properties with a focus on the impact of biomass burning are studied over Cape Town using data from the Aerosol Robotic Network (AERONET) and the Moderate Resolution Imaging Spectroradiometer (MODIS). In general terms, measurements from both platforms significantly agree on the estimates of aerosol optical depth (AOD) and water vapor content. The mean AOD (0.075 ± 0.022) and the Ångström exponent (0.63 ± 0.19) derived from AERONET demonstrate the dominance of coarse mode aerosol typical of maritime aerosol. Similarly, aerosol particle size distributions display the predominance of coarse mode particles. However, the derived refractive index is more representative of urban-industrial aerosol. Also, estimated back-trajectories show that more than 70% of the aerosol particles over the region originate over the ocean. Atmospheric vapor increases from winter to summer, mainly influenced by air temperature, supersaturation level, and absorbing aerosol. Furthermore, two significant sources accounted for biomass burning related to high AOD values: local biomass burning and regionally transported aged smoke majorly from elsewhere in Sothern Africa. 2021 artículo científico 0187-6236 https://www.redalyc.org/articulo.oa?id=56572302003 https://www.redalyc.org/journal/565/56572302003/ https://www.redalyc.org/journal/565/56572302003/html/ https://www.redalyc.org/journal/565/56572302003/56572302003.epub https://www.redalyc.org/journal/565/56572302003/movil 10.20937/ATM.52811 en http://www.redalyc.org/revista.oa?id=565 Atmósfera application/pdf Universidad Nacional Autónoma de México Atmósfera (México) Num.4 Vol.34 |
| title | Optical properties of atmospheric aerosol over Cape Town, Western Cape of South Africa: Role of biomass burning |
| topic | Biología back trajectory biomass burning fire radiative power Aerosol optical depth |
| url | https://www.redalyc.org/articulo.oa?id=56572302003 https://www.redalyc.org/journal/565/56572302003/ https://www.redalyc.org/journal/565/56572302003/html/ https://www.redalyc.org/journal/565/56572302003/56572302003.epub https://www.redalyc.org/journal/565/56572302003/movil |