Atmos. Chem. Phys. Discuss., 13, 19583-19623, 2013
www.atmos-chem-phys-discuss.net/13/19583/2013/
doi:10.5194/acpd-13-19583-2013
© Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
A parameterization of sub-grid particle formation in sulphur-rich plumes for global and regional-scale models
R. G. Stevens1 and J. R. Pierce1,2
1Department of Physics and Atmospheric Science, Dalhousie University, Halifax, NS, Canada
2Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA

Abstract. New-particle formation in the plumes of coal-fired power plants and other anthropogenic sulphur sources may be an important source of particles in the atmosphere. It remains unclear, however, how best to reproduce this formation in global and regional aerosol models with grid-box lengths that are tens of kilometres and larger. Based on the results of the System for Atmospheric Modelling (SAM), a Large-Eddy Simulation/Cloud-Resolving Model (LES/CRM) with online TwO Moment Aerosol Sectional (TOMAS) microphysics, we have developed a computationally efficient, but physically based, parameterization that predicts the characteristics of aerosol formed within sulphur-rich plumes based on parameters commonly available in global- and regional-scale models. Given large-scale mean meteorological parameters ((1) wind speed, (2) boundary-layer height and (3) downward shortwave radiative flux), (4) emissions of SO2 and (5) NOx from the source, (6) mean background condensation sink, (7) background SO2 and (8) NOx concentrations, and (9) the desired distance from the source; the parameterization will predict: (1) the fraction of the emitted SO2 that is oxidized to H2SO4, (2) the fraction of that H2SO4 that forms new particles instead of condensing onto preexisting particles, (3) the mean mass per particle of the newly formed particles, and (4) the number of newly formed particles per kilogram SO2 emitted. The parameterization we describe here should allow for more accurate predictions of aerosol size distributions and a greater confidence in the effects of aerosols in climate and health studies.

Citation: Stevens, R. G. and Pierce, J. R.: A parameterization of sub-grid particle formation in sulphur-rich plumes for global and regional-scale models, Atmos. Chem. Phys. Discuss., 13, 19583-19623, doi:10.5194/acpd-13-19583-2013, 2013.
 
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