Articles | Volume 20, issue 8
https://doi.org/10.5194/acp-20-4561-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-20-4561-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
20 Apr 2020
Research article |
| 20 Apr 2020
| 20 Apr 2020
Seasonal source variability of carbonaceous aerosols at the Rwanda Climate Observatory
August Andersson
CORRESPONDING AUTHOR
Department of Environmental Science and the Bolin Centre for Climate
Research, Stockholm University, 10691 Stockholm, Sweden
Elena N. Kirillova
Department of Environmental Science and the Bolin Centre for Climate
Research, Stockholm University, 10691 Stockholm, Sweden
Institute of Atmospheric Sciences and Climate (ISAC), National Research
Council of Italy, Bologna, Italy
Stefano Decesari
Institute of Atmospheric Sciences and Climate (ISAC), National Research
Council of Italy, Bologna, Italy
Langley DeWitt
Center for Global Change Science, Massachusetts Institute of
Technology, Cambridge, MA, USA
Jimmy Gasore
Center for Global Change Science, Massachusetts Institute of
Technology, Cambridge, MA, USA
Climate Secretariat, Ministry of Education, Kigali, Rwanda
Physics Department, School of Physics, College of Science and
Technology, University of Rwanda, Kigali, Rwanda
Katherine E. Potter
Center for Global Change Science, Massachusetts Institute of
Technology, Cambridge, MA, USA
Ronald G. Prinn
Center for Global Change Science, Massachusetts Institute of
Technology, Cambridge, MA, USA
Maheswar Rupakheti
Institute for Advanced Sustainability Studies (IASS), Potsdam,
Germany
Jean de Dieu Ndikubwimana
Climate Secretariat, Ministry of Education, Kigali, Rwanda
Julius Nkusi
Climate Secretariat, Ministry of Education, Kigali, Rwanda
Bonfils Safari
Physics Department, School of Physics, College of Science and
Technology, University of Rwanda, Kigali, Rwanda
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Cited
10 citations as recorded by crossref.
- Non‐Fossil Origin Explains the Large Seasonal Variation of Highly Processed Organic Aerosol in the Northeastern Tibetan Plateau (3,200 m a.s.l.) H. Ni et al. 10.1029/2023GL104710
- Black carbon aerosols over Indian Ocean have unique source fingerprint and optical characteristics during monsoon season K. Budhavant et al. 10.1073/pnas.2210005120
- Atmospheric Black Carbon Loadings and Sources over Eastern Sub-Saharan Africa Are Governed by the Regional Savanna Fires L. Kirago et al. 10.1021/acs.est.2c05837
- Organic aerosol formation and aging processes in Beijing constrained by size-resolved measurements of radiocarbon and stable isotopic 13C H. Ni et al. 10.1016/j.envint.2021.106890
- Sources and long-term variability of carbon monoxide at Mount Kenya and in Nairobi L. Kirago et al. 10.5194/acp-23-14349-2023
- 14C characteristics of organic carbon in the atmosphere and at glacier region of the Tibetan Plateau C. Li et al. 10.1016/j.scitotenv.2022.155020
- Black carbon emissions from traffic contribute substantially to air pollution in Nairobi, Kenya L. Kirago et al. 10.1038/s43247-022-00400-1
- Stable carbon isotopic composition of biomass burning emissions – implications for estimating the contribution of C<sub>3</sub> and C<sub>4</sub> plants R. Vernooij et al. 10.5194/acp-22-2871-2022
- Detailed Carbon Isotope Study of PM2.5 Aerosols at Urban Background, Suburban Background and Regional Background Sites in Hungary I. Major et al. 10.3390/atmos13050716
- NMR spectroscopic applications to atmospheric organic aerosol analysis – Part 1: A critical review of data source and analysis, potentialities and limitations S. Decesari et al. 10.1016/j.trac.2023.117516
10 citations as recorded by crossref.
- Non‐Fossil Origin Explains the Large Seasonal Variation of Highly Processed Organic Aerosol in the Northeastern Tibetan Plateau (3,200 m a.s.l.) H. Ni et al. 10.1029/2023GL104710
- Black carbon aerosols over Indian Ocean have unique source fingerprint and optical characteristics during monsoon season K. Budhavant et al. 10.1073/pnas.2210005120
- Atmospheric Black Carbon Loadings and Sources over Eastern Sub-Saharan Africa Are Governed by the Regional Savanna Fires L. Kirago et al. 10.1021/acs.est.2c05837
- Organic aerosol formation and aging processes in Beijing constrained by size-resolved measurements of radiocarbon and stable isotopic 13C H. Ni et al. 10.1016/j.envint.2021.106890
- Sources and long-term variability of carbon monoxide at Mount Kenya and in Nairobi L. Kirago et al. 10.5194/acp-23-14349-2023
- 14C characteristics of organic carbon in the atmosphere and at glacier region of the Tibetan Plateau C. Li et al. 10.1016/j.scitotenv.2022.155020
- Black carbon emissions from traffic contribute substantially to air pollution in Nairobi, Kenya L. Kirago et al. 10.1038/s43247-022-00400-1
- Stable carbon isotopic composition of biomass burning emissions – implications for estimating the contribution of C<sub>3</sub> and C<sub>4</sub> plants R. Vernooij et al. 10.5194/acp-22-2871-2022
- Detailed Carbon Isotope Study of PM2.5 Aerosols at Urban Background, Suburban Background and Regional Background Sites in Hungary I. Major et al. 10.3390/atmos13050716
- NMR spectroscopic applications to atmospheric organic aerosol analysis – Part 1: A critical review of data source and analysis, potentialities and limitations S. Decesari et al. 10.1016/j.trac.2023.117516
Latest update: 23 Nov 2024
Short summary
Large-scale biomass burning events seasonally cover sub-Saharan Africa with air particles. In this study, we find that the concentrations of these particles at a remote mountain site in Rwanda may increase by a factor of 10 during such dry biomass burning periods, with strong implications for the regional climate and human health. These results provide quantitative constraints that could contribute to reducing the large uncertainties regarding the environmental impact of these fires.
Large-scale biomass burning events seasonally cover sub-Saharan Africa with air particles. In...
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