Using Novel Molecular-Level Chemical Composition Observations of High Arctic Organic Aerosol for Predictions of Cloud Condensation Nuclei

[Image: see text] Predictions of cloud droplet activation in the late summertime (September) central Arctic Ocean are made using κ-Köhler theory with novel observations of the aerosol chemical composition from a high-resolution time-of-flight chemical ionization mass spectrometer with a filter inlet...

Full description

Bibliographic Details
Published in:Environmental Science & Technology
Main Authors: Siegel, Karolina, Neuberger, Almuth, Karlsson, Linn, Zieger, Paul, Mattsson, Fredrik, Duplessis, Patrick, Dada, Lubna, Daellenbach, Kaspar, Schmale, Julia, Baccarini, Andrea, Krejci, Radovan, Svenningsson, Birgitta, Chang, Rachel, Ekman, Annica M. L., Riipinen, Ilona, Mohr, Claudia
Format: Text
Language:English
Published: American Chemical Society 2022
Subjects:
Aitken
Arctic
Arctic Ocean
oden
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9535938/
http://www.ncbi.nlm.nih.gov/pubmed/36112784
https://doi.org/10.1021/acs.est.2c02162
Description
Summary:[Image: see text] Predictions of cloud droplet activation in the late summertime (September) central Arctic Ocean are made using κ-Köhler theory with novel observations of the aerosol chemical composition from a high-resolution time-of-flight chemical ionization mass spectrometer with a filter inlet for gases and aerosols (FIGAERO-CIMS) and an aerosol mass spectrometer (AMS), deployed during the Arctic Ocean 2018 expedition onboard the Swedish icebreaker Oden. We find that the hygroscopicity parameter κ of the total aerosol is 0.39 ± 0.19 (mean ± std). The predicted activation diameter of ∼25 to 130 nm particles is overestimated by 5%, leading to an underestimation of the cloud condensation nuclei (CCN) number concentration by 4–8%. From this, we conclude that the aerosol in the High Arctic late summer is acidic and therefore highly cloud active, with a substantial CCN contribution from Aitken mode particles. Variability in the predicted activation diameter is addressed mainly as a result of uncertainties in the aerosol size distribution measurements. The organic κ was on average 0.13, close to the commonly assumed κ of 0.1, and therefore did not significantly influence the predictions. These conclusions are supported by laboratory experiments of the activation potential of seven organic compounds selected as representative of the measured aerosol.

Similar Items