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Volume 15, issue 3
Atmos. Chem. Phys., 15, 1367-1383, 2015
https://doi.org/10.5194/acp-15-1367-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 15, 1367-1383, 2015
https://doi.org/10.5194/acp-15-1367-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 09 Feb 2015

Research article | 09 Feb 2015

Size-resolved observations of refractory black carbon particles in cloud droplets at a marine boundary layer site

J. C. Schroder1, S. J. Hanna1, R. L. Modini2, A. L. Corrigan2, S. M. Kreidenwies6, A. M. Macdonald3, K. J. Noone5, L. M. Russell2, W. R. Leaitch4, and A. K. Bertram1 J. C. Schroder et al.
  • 1Department of Chemistry, University of British Columbia, Vancouver, BC, V6T 1Z1, Canada
  • 2Scripps Institute of Oceanography, University of California-San Diego, La Jolla, San Diego, CA, USA
  • 3Air Quality Processes Research Section, Environment Canada, Toronto, ON, Canada
  • 4Climate Chemistry and Measurements Research, Environment Canada, Toronto, ON, Canada
  • 5Department of Applied Environmental Science, Stockholm University, Stockholm, Sweden
  • 6Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA

Abstract. Size-resolved observations of aerosol particles and cloud droplet residuals were studied at a marine boundary layer site (251 m a.m.s.l.) in La Jolla, San Diego, California, during 2012. A counterflow virtual impactor (CVI) was used as the inlet to sample cloud residuals while a total inlet was used to sample both cloud residuals and interstitial particles. Two cloud events totaling 10 h of in-cloud sampling were analyzed. Based on bulk aerosol particle concentrations, mass concentrations of refractory black carbon (rBC), and back trajectories, the two air masses sampled were classified as polluted marine air. Since the fraction of cloud droplets sampled by the CVI was less than 100%, the measured activated fractions of rBC should be considered as lower limits to the total fraction of rBC activated during the two cloud events. Size distributions of rBC and a coating analysis showed that sub-100 nm rBC cores with relatively thick coatings were incorporated into the cloud droplets (i.e., 95 nm rBC cores with median coating thicknesses of at least 65 nm were incorporated into the cloud droplets). Measurements also show that the coating volume fraction of rBC cores is relatively large for sub-100 nm rBC cores. For example, the median coating volume fraction of 95 nm rBC cores incorporated into cloud droplets was at least 0.9, a result that is consistent with κ-Köhler theory. Measurements of the total diameter of the rBC-containing particles (rBC core and coating) suggest that the total diameter of rBC-containing particles needed to be at least 165 nm to be incorporated into cloud droplets when the core rBC diameter is ≥ 85 nm. This result is consistent with previous work that has shown that particle diameter is important for activation of non-rBC particles. The activated fractions of rBC determined from the measurements ranged from 0.01 to 0.1 for core rBC diameters ranging from 70 to 220 nm. This type of data is useful for constraining models used for predicting rBC concentrations in the atmosphere.

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