Rapid changes in biomass burning aerosols by atmospheric oxidation

V. Vakkari,V. Kerminen,J. Beukes,P. Tiitta,P. Zyl,M. Josipovic,A. Venter,K. Jaars,D. Worsnop,M. Kulmala,L. Laakso

Published 2014 in Geophysical Research Letters

ABSTRACT

Primary and secondary aerosol particles originating from biomass burning contribute significantly to the atmospheric aerosol budget and thereby to both direct and indirect radiative forcing. Based on detailed measurements of a large number of biomass burning plumes of variable age in southern Africa, we show that the size distribution, chemical composition, single‐scattering albedo, and hygroscopicity of biomass burning particles change considerably during the first 2–4 h of their atmospheric transport. These changes, driven by atmospheric oxidation and subsequent secondary aerosol formation, may reach a factor of 6 for the aerosol scattering coefficient and a factor >10 for the cloud condensation nuclei concentration. Since the observed changes take place over the spatial and temporal scales that are neither covered by emission inventories nor captured by large‐scale model simulations, the findings reported here point out a significant gap in our understanding on the climatic effects of biomass burning aerosols.

PUBLICATION RECORD

  • Publication year

    2014

  • Venue

    Geophysical Research Letters

  • Publication date

    2014-04-16

  • Fields of study

    Geology, Environmental Science

  • Identifiers
  • External record

    Open on Semantic Scholar

  • Source metadata

    Semantic Scholar

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