Heterogeneous ice nucleation properties of natural desert dust particles coated with a surrogate of secondary organic aerosol

• Main Authors: Z. A. Kanji, R. C. Sullivan, M. Niemand, P. J. DeMott, A. J. Prenni, C. Chou, H. Saathoff, O. Möhler
• Format: Article
• Language: English
• Published: Copernicus Publications 2019-04-01
• Series: Atmospheric Chemistry and Physics
• Online Access: https://www.atmos-chem-phys.net/19/5091/2019/acp-19-5091-2019.pdf

<p>Ice nucleation abilities of surface collected mineral dust particles from the Sahara (SD) and Asia (AD) are investigated for the temperature (<span class="inline-formula"><i>T</i></span>) range 253–233&thinsp;K and for supersaturated relative humidity (RH) conditions in the immersion freezing regime. The dust particles were also coated with a proxy of secondary organic aerosol (SOA) from the dark ozonolysis of <span class="inline-formula"><i>α</i></span>-pinene to better understand the influence of atmospheric coatings on the immersion freezing ability of mineral dust particles. The measurements are conducted on polydisperse particles in the size range 0.01–3&thinsp;<span class="inline-formula">µ</span>m with three different ice nucleation chambers. Two of the chambers follow the continuous flow diffusion chamber (CFDC) principle (Portable Ice Nucleation Chamber, PINC) and the Colorado State University CFDC (CSU-CFDC), whereas the third was the Aerosol Interactions and Dynamics in the Atmosphere (AIDA) cloud expansion chamber. From observed activated fractions (<i>AFs</i>) and ice nucleation active site (<i>INAS</i>) <i>densities</i>, it is concluded within experimental uncertainties that there is no significant difference between the ice nucleation ability of the particular SD and AD samples examined. A small bias towards higher <i>INAS densities</i> for uncoated versus SOA-coated dusts is found but this is well within the 1<span class="inline-formula"><i>σ</i></span> (66&thinsp;% prediction bands) region of the average fit to the data, which captures 75&thinsp;% of the <i>INAS densities</i> observed in this study. Furthermore, no systematic differences are observed between SOA-coated and uncoated dusts in both SD and AD cases, regardless of coating thickness (3–60&thinsp;nm). The results suggest that any differences observed are within the uncertainty of the measurements or differences in cloud chamber parameters such as size fraction of particles sampled, and residence time, as well as assumptions in using <i>INAS densities</i> to compare polydisperse aerosol measurements which may show variable composition with particle size. Coatings with similar properties to that of the SOA in this work and with coating thickness up to 60&thinsp;nm are not expected to impede or enhance the immersion mode ice nucleation ability of mineral dust particles.</p>