Poster's note : of particular relevance to marine cloud brightening

http://onlinelibrary.wiley.com/doi/10.1002/jgrd.50325/abstract

Keywords:

heterogeneous ice nucleation;sodium chloride dihydrate;sea salt aerosol

Abstract

The aerosol and cloud chamber AIDA (Aerosol Interactions and Dynamics in
the Atmosphere) of the Karlsruhe Institute of Technology has been used to
quantify the deposition mode ice nucleation ability of airborne crystalline
sodium chloride dihydrate (NaCl ∙ 2H2O) particles with median diameters
between 0.06 and 1.1 µm. For this purpose, expansion cooling experiments
with starting temperatures from 235 to 216 K were conducted. Recently,
supermicron-sized NaCl ∙ 2H2O particles deposited onto a surface have been
observed to be ice-active in the deposition mode at temperatures below 238
K, requiring a median threshold ice saturation ratio of only 1.02 in the
range from 238 to 221 K. In AIDA, heterogeneous ice nucleation by NaCl ∙
2H2O was first detected at a temperature of 227.1 K with a concomitant
threshold ice saturation ratio of 1.25. Above that temperature, the
crystallized salt particles underwent a deliquescence transition to form
aqueous NaCl solution droplets upon increasing relative humidity. At
nucleation temperatures below 225 K, the inferred threshold ice saturation
ratios varied between 1.15 and 1.20. The number concentration of the
nucleated ice crystals was related to the surface area of the seed aerosol
particles to deduce the ice nucleation active surface site (INAS) density
of the aerosol population as a function of the ice supersaturation. Maximum
INAS densities of about 6 ⋅ 1010 m−2 at an ice saturation ratio of 1.20
were found for temperatures below 225 K. These INAS densities are similar
to those recently derived for deposition mode ice nucleation on mineral
dust particles.

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