Experimental Study on the Dependency of Ice Nucleation Active Surface Site Density on ATD Aerosol Size

Abstract

In light of the percentage of Earth’s cloud coverage, heterogeneous ice nucleation in clouds is the most important global-scale pathway. More recent parameterizations of ice nucleation processes in the atmosphere are based on the concept of ice nucleation active surface site density ( n s ). It is usually assumed that n s is independent of time and aerosol size distribution, i.e. that the surface properties of aerosols of the same species do not vary with size. However, the independence of n s on aerosol size for every species has been questioned. This study presents the results of ice nucleation processes of ATD laboratory-generated aerosol (particle diameters of 0 - 3 μm). Ice nucleation in the condensation mode was performed in a Dynamic Filter Processing Cham- ber at temperatures of - 18 ° C and - 22 ° C, with a saturation ratio with respect to water of 1.02. Results show that n s increased by lowering the nucleation temperature, and was also dependent on the particle size. The n s of particles collected on the filters, after a 0.5 μm D 50 cut-off cyclone, resulted statistically higher with respect to the values obtained from the particles collected on total filters. The results obtained suggest the need for further investigation of n s dependence of same composition aerosol particles with a view to support weather and climate predictions.