Articles | Volume 15, issue 5
https://doi.org/10.5194/acp-15-2545-2015
https://doi.org/10.5194/acp-15-2545-2015
Research article
 | 
06 Mar 2015
Research article |  | 06 Mar 2015

Importance of aerosol composition and mixing state for cloud droplet activation over the Arctic pack ice in summer

C. Leck and E. Svensson

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Cited articles

Abbatt, J. P. D., Broekhuizen, K., and Pradeep Kumar, P.: Cloud condensation nucleus activity of internally mixed ammonium sulfate/organic acid aerosol particles, Atmos. Environ., 39, 4767–4778, 2005.
Bigg, E. K. and Leck, C.: Cloud-active particles over the central Arctic Ocean, J. Geophys. Res., 106, 32155–32166, 2001a.
Bigg, E. K. and Leck, C.: Properties of the aerosol over the central Arctic Ocean, J. Geophys. Res., 106, 32101–32109, 2001b.
Bigg, E. K. and Leck, C.: The composition of fragments of bubbles bursting at the ocean surface, J. Geophys. Res., 113, 1209, https://doi.org/10.1029/2007JD009078, 2008.
Bigg, E. K., Leck, C., and Nilsson, E. D.: Sudden changes in arctic atmospheric aerosol concentrations during summer and autumn, Tellus, 48B, 254–271, 1996.
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In the Arctic clouds are very important for determining the melting of the sea ice. The radiative properties of the optically thin Arctic clouds strongly depend on the number of particles available for water uptake. This study argues that the Köhler equation commonly used for simulating cloud droplet activation is not fully complete for describing the condensational growth of the interaction of the hydrophilic and hydrophobic entities on the structures of the airborne polymer gels present.
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