Ice-nucleating particles active below -24 °C in a Finnish boreal forest and their relationship to bioaerosols

• DOI: 10.5194/egusphere-2024-853
• Publication Date: 2024-04-09T08:05:04Z
• Authors: Franziska Vogel; Michael P. Adams; Larissa Lacher; Polly Foster; Grace C. E. Porter; Barbara Bertozzi; Kristina Höhler; Julia Schneider; Tobias Schorr; Nsikanabasi S. Umo; Jens Nadolny; Zoé Brasseur; Paavo Heikkilä; Erik S. Thomson; Nicole Büttner; Martin I. Daily; Romy Fösig; Alexander D. Harr...; Jorma Keskinen; Ulrike Proske; Jonathan Duplissy; Markku Kulmala; Tuukka Petäjä; Ottmar Möhler; Benjamin J. Murray
• Keywords: info:eu-repo/classification/ddc/550; Ash particles; 330; 550; Biogenic aerosol; ddc:550; Climate; Physics; QC1-999; Field; Mineral dust; Agronomy; Physical sciences; Earth sciences; Chemistry; Lichen soredia; Life Science; Biological aerosol-particles; Nuclei populations; QD1-999; Mixed-phase; Sea-surface microlayer

Abstract. Cloud properties are strongly influenced by ice formation, hence we need to understand the sources of ice-nucleating particles (INPs) around the globe. Boreal forests are known as sources of bioaerosol and recent work indicates that these dominate the INP spectra above -24 °C. To quantify the INP population at temperatures below -24 °C, we deployed a portable cloud expansion chamber (PINE) in a Finnish boreal forest from March 13, 2018 to May 11, 2018. Using the 6 min time resolution PINE data, we present several lines of evidence that INPs below -24 °C in this location are also from biological sources: an INP parameterization developed for a pine forest site in Colorado, where many INPs were shown to be biological, produced a good fit to our measurements; a moderate correlation of INP with aerosol concentration larger than 0.5 μm and the fluorescent bioaerosol concentration; a negative correlation with relative humidity that may relate to enhanced release of bioaerosol at low humidity from local sources such as the prolific lichen population in boreal forests. The absence of correlation with ultrafine particles (3.5 to 50 nm) indicates that new particle formation events are not sources of INP. This study should motivate further work to establish if the commonality in bioaerosol ice nucleating properties between spring in Finland and summer in Colorado is more generally applicable to different coniferous forest locations and times, and also to determine to what extent these bioaerosols are transported to locations where they may affect clouds.