Articles | Volume 16, issue 12
https://doi.org/10.5194/acp-16-7709-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-7709-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The evolution of biomass-burning aerosol size distributions due to coagulation: dependence on fire and meteorological details and parameterization
Kimiko M. Sakamoto
Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA
James R. Laing
School of Science and Technology, University of Washington-Bothell, Bothell, WA, USA
Robin G. Stevens
School of Earth and Environment, University of Leeds, Leeds, UK
Daniel A. Jaffe
School of Science and Technology, University of Washington-Bothell, Bothell, WA, USA
Department of Atmospheric Science, University of Washington, Seattle, WA, USA
Jeffrey R. Pierce
CORRESPONDING AUTHOR
Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA
Department of Physics and Atmospheric Science, Dalhousie University, Halifax, NS, Canada
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- More Than Emissions and Chemistry: Fire Size, Dilution, and Background Aerosol Also Greatly Influence Near‐Field Biomass Burning Aerosol Aging A. Hodshire et al. 10.1029/2018JD029674
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Latest update: 21 Nov 2024
Short summary
We determine how various meteorological and fire factors contribute to shaping the aged biomass-burning particle size distribution through coagulation. The mass emissions flux, fire area, and wind speed are dominant factors controlling the aged size distribution. We parameterize the aged size distribution for global/regional aerosol models. We estimate that the aged biomass-burning particle size distribution may be more sensitive to variability in coagulation than SOA formation.
We determine how various meteorological and fire factors contribute to shaping the aged...
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