Regional Influence of Aerosol Emissions from Wildfires Driven by Combustion Efficiency: Insights from the BBOP Campaign

  • Sonya Collier
  • , Shan Zhou
  • , Timothy B. Onasch
  • , Daniel A. Jaffe
  • , Lawrence Kleinman
  • , Arthur J. Sedlacek
  • , Nicole L. Briggs
  • , Jonathan Hee
  • , Edward Fortner
  • , John E. Shilling
  • , Douglas Worsnop
  • , Robert J. Yokelson
  • , Caroline Parworth
  • , Xinlei Ge
  • , Jianzhong Xu
  • , Zachary Butterfield
  • , Duli Chand
  • , Manvendra K. Dubey
  • , Mikhail S. Pekour
  • , Stephen Springston
  • Qi Zhang

Research output: Contribution to journalArticlepeer-review

101 Scopus citations

Abstract

Wildfires are important contributors to atmospheric aerosols and a large source of emissions that impact regional air quality and global climate. In this study, the regional and nearfield influences of wildfire emissions on ambient aerosol concentration and chemical properties in the Pacific Northwest region of the United States were studied using real-time measurements from a fixed ground site located in Central Oregon at the Mt. Bachelor Observatory (∼2700 m a.s.l.) as well as near their sources using an aircraft. The regional characteristics of biomass burning aerosols were found to depend strongly on the modified combustion efficiency (MCE), an index of the combustion processes of a fire. Organic aerosol emissions had negative correlations with MCE, whereas the oxidation state of organic aerosol increased with MCE and plume aging. The relationships between the aerosol properties and MCE were consistent between fresh emissions (∼1 h old) and emissions sampled after atmospheric transport (6-45 h), suggesting that biomass burning organic aerosol concentration and chemical properties were strongly influenced by combustion processes at the source and conserved to a significant extent during regional transport. These results suggest that MCE can be a useful metric for describing aerosol properties of wildfire emissions and their impacts on regional air quality and global climate.

Original languageEnglish
Pages (from-to)8613-8622
Number of pages10
JournalEnvironmental Science and Technology
Volume50
Issue number16
DOIs
StatePublished - Aug 16 2016

Funding

This work was funded by US Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) program and the Atmospheric System Research (ASR) program (Grants DESC0014620, DE-SC0007178, and DE-SC0014287) and used data from the ARM Climate Research Facility, a DOE Office of Science User Facility. MBO receives funding from the National Science Foundation (Grant NSF-1447832 to DJ). R.Y. was supported by NASA ACCDAM award NNX14AP45G. The Pacific Northwest National Laboratory is operated for DOE by Battelle Memorial Institute under contract DE-AC05- 76RL01830. MKD thanks ASR grant F265 for support to LANL.

FundersFunder number
1447832, NSF-1447832
DE-SC0007178, DE-SC0014287, DESC0014620
National Aeronautics and Space AdministrationNNX14AP45G
BattelleDE-AC05- 76RL01830, F265

    UN SDGs

    This output contributes to the following UN Sustainable Development Goals (SDGs)

    1. SDG 13 - Climate Action
      SDG 13 Climate Action

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