Journal article
Biomass burning dominates brown carbon absorption in the rural southeastern United States
Geophysical Research Letters, Vol.42(2), pp.653-664
01/28/2015
DOI: 10.1002/2014GL062444
Abstract
Brown carbon aerosol consists of light‐absorbing organic particulate matter with wavelength‐dependent absorption. Aerosol optical extinction, absorption, size distributions, and chemical composition were measured in rural Alabama during summer 2013. The field site was well located to examine sources of brown carbon aerosol, with influence by high biogenic organic aerosol concentrations, pollution from two nearby cities, and biomass burning aerosol. We report the optical closure between measured dry aerosol extinction at 365 nm and calculated extinction from composition and size distribution, showing agreement within experiment uncertainties. We find that aerosol optical extinction is dominated by scattering, with single‐scattering albedo values of 0.94 ± 0.02. Black carbon aerosol accounts for 91 ± 9% of the total carbonaceous aerosol absorption at 365 nm, while organic aerosol accounts for 9 ± 9%. The majority of brown carbon aerosol mass is associated with biomass burning, with smaller contributions from biogenically derived secondary organic aerosol.
Key Points
- Aerosol optical extinction in the southeastern U.S. is dominated by scattering
- Black carbon is a more significant absorber than organic carbon at 365 nm
- Biomass burning makes the largest contribution to organic aerosol absorption
Details
- Title: Subtitle
- Biomass burning dominates brown carbon absorption in the rural southeastern United States
- Creators
- C. A Brock - National Oceanic and Atmospheric AdministrationH Guo - Georgia Institute of TechnologyL Xu - Georgia Institute of TechnologyR. J Weber - Georgia Institute of TechnologyN. L Ng - Georgia Institute of TechnologyH. M Allen - California Institute of TechnologyB R Ayres - Reed CollegeK Baumann - Atmospheric Research & Analysis, IncR. C Cohen - University of CaliforniaD. C Draper - University of CaliforniaK. C Duffey - University of CaliforniaE Edgerton - Atmospheric Research & Analysis, IncJ. L Fry - Reed CollegeW. W Hu - University of Colorado BoulderJ. L Jimenez - University of Colorado BoulderB. B Palm - University of Colorado BoulderP Romer - University of CaliforniaE. A Stone - University of Iowa, ChemistryP. J Wooldridge - University of CaliforniaR. A Washenfelder - National Oceanic and Atmospheric AdministrationA. R Attwood - Now at Horiba ScientificS S Brown - University of Colorado Boulder
- Resource Type
- Journal article
- Publication Details
- Geophysical Research Letters, Vol.42(2), pp.653-664
- DOI
- 10.1002/2014GL062444
- ISSN
- 0094-8276
- eISSN
- 1944-8007
- Number of pages
- 12
- Grant note
- NOAA (NA13OAR4310063) Office of Biological and Environmental Research (DE‐SC0011105) National Science Foundation (1243354) EPA (STAR‐83540101)
- Language
- English
- Date published
- 01/28/2015
- Academic Unit
- Chemistry; Chemical and Biochemical Engineering
- Record Identifier
- 9983985858002771
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