Abstract

Abstract. This study reports laboratory measurements of particle size distributions, cloud condensation nuclei (CCN) activity, and droplet activation kinetics of wet generated aerosols from clays, calcite, quartz, and desert soil samples from Northern Africa, East Asia/China, and Northern America. The dependence of critical supersaturation, sc, on particle dry diameter, Ddry, is used to characterize particle-water interactions and assess the ability of Frenkel-Halsey-Hill adsorption activation theory (FHH-AT) and Köhler theory (KT) to describe the CCN activity of the considered samples. Wet generated regional dust samples produce unimodal size distributions with particle sizes as small as 40 nm, CCN activation consistent with KT, and exhibit hygroscopicity similar to inorganic salts. Wet generated clays and minerals produce a bimodal size distribution; the CCN activity of the smaller mode is consistent with KT, while the larger mode is less hydrophilic, follows activation by FHH-AT, and displays almost identical CCN activity to dry generated dust. Ion Chromatography (IC) analysis performed on regional dust samples indicates a soluble fraction that cannot explain the CCN activity of dry or wet generated dust. A mass balance and hygroscopicity closure suggests that the small amount of ions (from low solubility compounds like calcite) present in the dry dust dissolve in the aqueous suspension during the wet generation process and give rise to the observed small hygroscopic mode. Overall these results identify an artifact that may question the atmospheric relevance of dust CCN activity studies using the wet generation method. Based on the method of threshold droplet growth analysis, wet generated mineral aerosols display similar activation kinetics compared to ammonium sulfate calibration aerosol. Finally, a unified CCN activity framework that accounts for concurrent effects of solute and adsorption is developed to describe the CCN activity of aged or hygroscopic dusts.

Highlights

  • The ability of aerosols to act as cloud condensation nuclei (CCN) can be characterized based on their size, chemical composition, and the level of water vapor supersaturation in ambient clouds

  • The CCN properties and droplet activation kinetics of aerosol wet generated from regional dust samples and individual minerals were measured

  • The aerosols were generated wet in the lab, and properties were measured using the Scanning Mobility CCN Analysis (Moore et al, 2010)

Read more

Summary

Introduction

The ability of aerosols to act as cloud condensation nuclei (CCN) can be characterized based on their size, chemical composition, and the level of water vapor supersaturation in ambient clouds. Mineral aerosol (or dust) has been recognized as an important atmospheric constituent because of its ability to act as CCN, giant CCN (GCCN) (e.g., Rosenfeld et al, 2001; Levin and Cotton, 2008), or ice nuclei (IN) (e.g., DeMott et al, 2003; Field et al, 2006). Dust particles are often transported over long distances downwind from their source regions During their transport, dust particles undergo atmospheric processing to form soluble species (like sulfates) on the dust surface (e.g., Levin et al, 1996) that have important impacts on dust CCN activity (Kelly et al, 2007)

Methods
Results
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call