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Volume 13, issue 9 | Copyright

Special issue: European Integrated Project on Aerosol-Cloud-Climate and Air...

Atmos. Chem. Phys., 13, 4917-4939, 2013
https://doi.org/10.5194/acp-13-4917-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 14 May 2013

Research article | 14 May 2013

The mass and number size distributions of black carbon aerosol over Europe

C. L. Reddington1, G. McMeeking2, G. W. Mann1, H. Coe3, M. G. Frontoso4, D. Liu3, M. Flynn3, D. V. Spracklen1, and K. S. Carslaw1 C. L. Reddington et al.
  • 1Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UK
  • 2Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA
  • 3School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester, UK
  • 4C2SM – ETH Zürich, Zürich, Switzerland

Abstract. Black carbon-containing aerosol particles play an important role in the direct and indirect radiative forcing of climate. However, the magnitude and sign of the net radiative effect is strongly dependent on the physical properties of the black carbon (BC) component of the particles, such as mass concentration, number size distribution and mixing state. Here we use a global aerosol model combined with aircraft measurements of BC particle number and size from the Single Particle Soot Photometer (SP2) to assess the realism with which these physical properties are predicted by global models. The comparison reveals a substantial mismatch between the measured and modelled BC size distribution over the size range of the SP2 instrument (90–400 nm BC diameter). The model predicts BC particle number concentrations a factor ~3.5–5.7 higher than measured and a mode diameter that is ~40–65 nm smaller than observed. More than ~90% of the model particles with dry diameters ≳260 nm contain BC, while the observations suggest only 14% on average. These model–observation biases in the BC properties are considerably greater than for the overall particle distribution, suggesting that the discrepancy is associated with model assumptions about the size and mixing state of the emitted carbonaceous particles. We expect the discrepancy in BC size distribution to be common among most global aerosol models, with implications for model estimates of absorption optical depth and direct radiative forcing.

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