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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 14, issue 14
Atmos. Chem. Phys., 14, 7431–7443, 2014
https://doi.org/10.5194/acp-14-7431-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 14, 7431–7443, 2014
https://doi.org/10.5194/acp-14-7431-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 18 Jul 2014

Research article | 18 Jul 2014

Black carbon concentrations and sources in the marine boundary layer of the tropical Atlantic Ocean using four methodologies

K. Pohl1, M. Cantwell2, P. Herckes3, and R. Lohmann1 K. Pohl et al.
  • 1Graduate School of Oceanography-University of Rhode Island, Narragansett, RI, USA
  • 2Environmental Protection Agency-Atlantic Ecology Division, Narragansett, RI, USA
  • 3Department of Chemistry and Biochemistry, Arizona State University, Tempe, AZ, USA

Abstract. Combustion-derived aerosols in the marine boundary layer have been poorly studied, especially in remote environments such as the open Atlantic Ocean. The tropical Atlantic has the potential to contain a high concentration of aerosols, such as black carbon, due to the African emission plume of biomass and agricultural burning products. Atmospheric particulate matter samples across the tropical Atlantic boundary layer were collected in the summer of 2010 during the southern hemispheric dry season when open fire events were frequent in Africa and South America. The highest black carbon concentrations were detected in the Caribbean Sea and within the African plume, with a regional average of 0.6 μg m−3 for both. The lowest average concentrations were measured off the coast of South America at 0.2 to 0.3 μg m−3. Samples were quantified for black carbon using multiple methods to provide insights into the form and stability of the carbonaceous aerosols (i.e., thermally unstable organic carbon, soot like, and charcoal like). Soot-like aerosols composed up to 45% of the carbonaceous aerosols in the Caribbean Sea to as little as 4% within the African plume. Charcoal-like aerosols composed up to 29% of the carbonaceous aerosols over the oligotrophic Sargasso Sea, suggesting that non-soot-like particles could be present in significant concentrations in remote environments. To better apportion concentrations and forms of black carbon, multiple detection methods should be used, particularly in regions impacted by biomass burning emissions.

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