Aerosol physicochemical effects on CCN activation simulated with the 
chemistry-climate model EMAC

Chang, D. Y.; Lelieveld, J.; Tost, H.; Steil, B.; Pozzer, A.; Yoon, J.

doi:10.1016/j.atmosenv.2017.03.036

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Aerosol physicochemical effects on CCN activation simulated with the chemistry-climate model EMAC

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Chang, D. Y.
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Lelieveld, J.
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Steil, B.
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

/persons/resource/persons101196

Pozzer, A.
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Citation

Chang, D. Y., Lelieveld, J., Tost, H., Steil, B., Pozzer, A., & Yoon, J. (2017). Aerosol physicochemical effects on CCN activation simulated with the chemistry-climate model EMAC. Atmospheric Environment, 162, 127-140. doi:10.1016/j.atmosenv.2017.03.036.

Cite as: https://hdl.handle.net/11858/00-001M-0000-002D-984A-C

Abstract

This study uses the EMAC atmospheric chemistry-climate model to simulate cloud properties with a prognostic cloud droplet nucleation scheme. We present modeled global distributions of cloud condensation nuclei (CCN) number concentrations and CCN activation rates, together with the effective hygroscopicity parameter κ, to describe the aerosol chemical composition effect on CCN activation. Large particles can easily activate into cloud droplets, even at low κ values due to the dominant size effect in cloud droplet formation. Small particles are less efficiently activated as CCN, and are more sensitive to aerosol composition and supersaturation. Since the dominant fraction of small particles generally originates from anthropogenic precursor emissions over land, this study focuses on the influence of the continental atmosphere, using a prognostic cloud droplet nucleation scheme that considers aerosol-cloud interactions during cloud formation, together with a double-moment cloud microphysics scheme. The agreement of simulated clouds and climate with observations generally improves over the Northern Hemisphere continents, particularly high air pollution regions such as Eastern US, Europe, East Asia by accounting for aerosol-cloud interactions that include impacts of chemical composition on CCN activation.