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...

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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:
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
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spelling ftpubmed:oai:pubmedcentral.nih.gov:9535938 2023-05-15T14:48:13+02:00 Using Novel Molecular-Level Chemical Composition Observations of High Arctic Organic Aerosol for Predictions of Cloud Condensation Nuclei 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 2022-09-16 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 en eng American Chemical Society http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9535938/ http://www.ncbi.nlm.nih.gov/pubmed/36112784 http://dx.doi.org/10.1021/acs.est.2c02162 © 2022 The Authors. Published by American Chemical Society https://creativecommons.org/licenses/by/4.0/Permits the broadest form of re-use including for commercial purposes, provided that author attribution and integrity are maintained (https://creativecommons.org/licenses/by/4.0/). CC-BY Environ Sci Technol Text 2022 ftpubmed https://doi.org/10.1021/acs.est.2c02162 2022-10-09T00:56:06Z [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. Text Arctic Arctic Ocean oden PubMed Central (PMC) Aitken ENVELOPE(-44.516,-44.516,-60.733,-60.733) Arctic Arctic Ocean Environmental Science & Technology 56 19 13888 13899
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
description [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.
format Text
author 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
spellingShingle 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
Using Novel Molecular-Level Chemical Composition Observations of High Arctic Organic Aerosol for Predictions of Cloud Condensation Nuclei
author_facet 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
author_sort Siegel, Karolina
title Using Novel Molecular-Level Chemical Composition Observations of High Arctic Organic Aerosol for Predictions of Cloud Condensation Nuclei
title_short Using Novel Molecular-Level Chemical Composition Observations of High Arctic Organic Aerosol for Predictions of Cloud Condensation Nuclei
title_full Using Novel Molecular-Level Chemical Composition Observations of High Arctic Organic Aerosol for Predictions of Cloud Condensation Nuclei
title_fullStr Using Novel Molecular-Level Chemical Composition Observations of High Arctic Organic Aerosol for Predictions of Cloud Condensation Nuclei
title_full_unstemmed Using Novel Molecular-Level Chemical Composition Observations of High Arctic Organic Aerosol for Predictions of Cloud Condensation Nuclei
title_sort using novel molecular-level chemical composition observations of high arctic organic aerosol for predictions of cloud condensation nuclei
publisher American Chemical Society
publishDate 2022
url 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
long_lat ENVELOPE(-44.516,-44.516,-60.733,-60.733)
geographic Aitken
Arctic
Arctic Ocean
geographic_facet Aitken
Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
oden
genre_facet Arctic
Arctic Ocean
oden
op_source Environ Sci Technol
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9535938/
http://www.ncbi.nlm.nih.gov/pubmed/36112784
http://dx.doi.org/10.1021/acs.est.2c02162
op_rights © 2022 The Authors. Published by American Chemical Society
https://creativecommons.org/licenses/by/4.0/Permits the broadest form of re-use including for commercial purposes, provided that author attribution and integrity are maintained (https://creativecommons.org/licenses/by/4.0/).
op_rightsnorm CC-BY
op_doi https://doi.org/10.1021/acs.est.2c02162
container_title Environmental Science & Technology
container_volume 56
container_issue 19
container_start_page 13888
op_container_end_page 13899
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