An attribution of the low single-scattering albedo of biomass burning aerosol over the southeastern Atlantic

Journal Article · 24 April 2023 · Atmospheric Chemistry and Physics (Online)

DOI: https://doi.org/10.5194/acp-23-4775-2023 · OSTI ID:1971263

Dobracki, Amie ^[1]; Zuidema, Paquita  ^[1]; Howell, Steven G. ^[2]; Saide, Pablo  ^[3]; Freitag, Steffen  ^[2]; Aiken, Allison C.  ^[4]; Burton, Sharon P. ^[5]; Sedlacek III, Arthur J.  ^[6]; Redemann, Jens  ^[7]; Wood, Robert  ^[8]

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1. Univ. of Miami, FL (United States)
2. Univ. of Hawaii at Manoa, Honolulu, HI (United States)
3. Univ. of California, Los Angeles, CA (United States)
4. Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
5. NASA Langley Research Center, Hampton, VA (United States)
6. Brookhaven National Laboratory (BNL), Upton, NY (United States)
7. Univ. of Oklahoma, Norman, OK (United States)
8. Univ. of Washington, Seattle, WA (United States)

Aerosol over the remote southeastern Atlantic is some of the most sunlight-absorbing aerosol on the planet: the in situ free-tropospheric single-scattering albedo at the 530 nm wavelength (SSA_{530 nm}) ranges from 0.83 to 0.89 within ORACLES (ObseRvations of Aerosols above CLouds and their intEractionS) aircraft flights from late August–September. Here we seek to explain the low SSA. The SSA depends strongly on the black carbon (BC) number fraction, which ranges from 0.15 to 0.4. Low organic aerosol (OA)-to-BC mass ratios of 8–14 and modified combustion efficiency values >0.975 point indirectly to the dry, flame-efficient combustion of primarily grass fuels, with back trajectories ending in the miombo woodlands of Angola. The youngest aerosol, aged 4–5 d since emission, occupied the top half of a 5 km thick plume sampled directly west of Angola with a vertically consistent BC:ΔCO (carbon monoxide) ratio, indicating a homogenization of the source emissions. The younger aerosol, transported more quickly off of the continent by stronger winds, overlaid older, slower-moving aerosol with a larger mean particle size and fraction of BC-containing particles. This is consistent with ongoing gas condensation and the coagulation of smaller non-BC particles upon the BC-containing particles. The particle volumes and OA:BC mass ratios of the older aerosol were smaller, attributed primarily to evaporation following fragmentation, instead of dilution or thermodynamics. The CLARIFY (CLoud–Aerosol–Radiation Interaction and Forcing: Year 2017) aircraft campaign sampled aerosols that had traveled further to reach the more remote Ascension Island. CLARIFY reported higher BC number fractions, lower OA:BC mass ratios, and lower SSA yet larger mass absorption coefficients compared to this study's. Values from one ORACLES 2017 flight, held midway to Ascension Island, are intermediate, confirming the long-range changes. Overall the data are most consistent with continuing oxidation through fragmentation releasing aerosols that subsequently enter the gas phase, reducing the OA mass, rather than evaporation through dilution or thermodynamics. The data support the following best fit: SSA_530nm=0.801+0055∙(OA:BC) (r=0.84). The fires of southern Africa emit approximately one-third of the world's carbon; the emitted aerosols are distinct from other regional smoke emissions, and their composition needs to be represented appropriately to realistically depict regional aerosol radiative effects.

• Research Organization: Brookhaven National Laboratory (BNL), Upton, NY (United States)
• Sponsoring Organization: USDOE Office of Science (SC), Biological and Environmental Research (BER); National Aeronautics and Space Administration (NASA); USDOE
• Grant/Contract Number: SC0012704; SC0021250; SC0018272; NNH13ZDA001N-EVS2; DESC0021250
• OSTI ID: 1971263
• Alternate ID(s): OSTI ID: 1984406
• Report Number(s): BNL-224453-2023-JAAM
• Journal Information: Atmospheric Chemistry and Physics (Online), Vol. 23, Issue 8; ISSN 1680-7324
• Publisher: Copernicus Publications, EGUCopyright Statement
• Country of Publication: United States
• Language: English