Atmos. Chem. Phys., 11, 2853-2861, 2011
www.atmos-chem-phys.net/11/2853/2011/
doi:10.5194/acp-11-2853-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
Size dependence of volume and surface nucleation rates for homogeneous freezing of supercooled water droplets
T. Kuhn1,*, M. E. Earle1,**, A. F. Khalizov1,***, and J. J. Sloan1
1Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, ON, Canada
*now at: Division of Space Technology, Department of Computer Science, Electrical and Space Engineering, Luleå University of Technology, Kiruna, Sweden
**now at: Cloud Physics and Severe Weather Research Section, Environment Canada, Toronto, ON, Canada
***now at: Department of Atmospheric Sciences, Texas A&M University, College Station, TX, USA

Abstract. The relative roles of volume and surface nucleation were investigated for the homogeneous freezing of pure water droplets. Experiments were carried out in a cryogenic laminar aerosol flow tube using supercooled water aerosols with maximum volume densities at radii between 1 and 3 μm. Temperature- and size-dependent values of volume- and surface-based homogeneous nucleation rates between 234.8 and 236.2 K were derived using a microphysical model and aerosol phase compositions and size distributions determined from infrared extinction measurements in the flow tube. The results show that the contribution from nucleation at the droplet surface increases with decreasing droplet radius and dominates over nucleation in the bulk droplet volume for droplets with radii smaller than approximately 5 μm. This is interpreted in terms of a lowered free energy of ice germ formation in the surface-based process. The implications of surface nucleation for the parameterization of homogeneous ice nucleation in numerical models are considered.

Citation: Kuhn, T., Earle, M. E., Khalizov, A. F., and Sloan, J. J.: Size dependence of volume and surface nucleation rates for homogeneous freezing of supercooled water droplets, Atmos. Chem. Phys., 11, 2853-2861, doi:10.5194/acp-11-2853-2011, 2011.
 
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