
Changes in aerosol size- and phase distributions due to physical and chemical processes in fog
Abstract
Measurements of the scavenging efficiency of aerosol particles in fog are presented. The scavenging efficiency as a function of size for accumulation-mode particles is presented, along with efficiencies for the total number, accumulation-mode number, and accumulation-mode volume. Particles below ca. 0.3 μm diameter were not efficiently scavenged in the fogs. The scavenging efficiency for accumulation-mode particles showed two steps, indicating that the hygroscopic/hydrophobic nature of the aerosol appeared to have been a controlling factor in determining scavenging efficiencies. Observed changes in the aerosol size distributions are discussed in reference to the processes (i.e., in-cloud scavenging, aqueous-phase reactions) potentially influencing them.
© 1992 Kevin J. Noone, John A. Ogren, Anneli Hallberg, Jost Heintzenberg, Johan Ström, Hans-Christen Hansson, Birgitta Svenningsson, Alfred Wiedensohler, Sandro Fuzzi, Maria Christina Facchini, Beate G. Arends, Axel Berner, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.