Abstract

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.

Highlights

  • Black carbon (BC) is the byproduct of the incomplete combustion of biomass and fossil fuels that is composed of highly condensed matrices of aromatic sheets (Goldberg, 1985)

  • We propose that Total organic carbon (TOC) concentrations in the marine boundary layer were a mix between degraded secondary organic aerosols from marine precursor volatile organic carbons, and primary organic aerosols ejected from sea spray (Keene et al, 2007; O’Dowd and Leeuw, 2007; Hodzic et al, 2010)

  • Black carbon particulates were collected in four sub-regions within the tropical Atlantic Ocean to determine the concentrations and distributions of combustion-derived aerosols in a remote and poorly sampled region

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Summary

Introduction

Black carbon (BC) is the byproduct of the incomplete combustion of biomass and fossil fuels that is composed of highly condensed matrices of aromatic sheets (Goldberg, 1985). It has the potential for long range atmospheric transport which makes it ubiquitous in the environment (Ogren and Charlson, 1983; Chuang et al, 2002; Masiello, 2004). Results are often extrapolated to estimate BC concentrations in these remote regions This uncertainty is further exacerbated by the fact that BC results are operationally defined by the selected analytical method (Schmidt et al, 2001; Andreae and Gelencser, 2006)

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