Impact of Biomass Burning on Arctic Aerosol Composition

Emissions from biomass burning (BB) occurring at midlatitudes can reach the Arctic, where they influence the remote aerosol population. By using measurements of levoglucosan and black carbon, we identify seven BB events reaching Svalbard in 2020. We find that most of the BB events are significantly...

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Main Authors: Gramlich, Yvette, Siegel, Karolina, Haslett, Sophie L., Cremer, Roxana S., Lunder, Chris, Kommula, Snehitha M., Buchholz, Angela, Yttri, Karl Espen, Chen, Gang, id_orcid:0 000-0002-1507-4622, Krejci, Radovan, Zieger, Paul, Virtanen, Annele, Riipinen, Ilona, Mohr, Claudia
Format: Article in Journal/Newspaper
Language:English
Published: American Chemical Society 2024
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/669616
https://doi.org/10.3929/ethz-b-000669616
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author Gramlich, Yvette
Siegel, Karolina
Haslett, Sophie L.
Cremer, Roxana S.
Lunder, Chris
Kommula, Snehitha M.
Buchholz, Angela
Yttri, Karl Espen
Chen, Gang
id_orcid:0 000-0002-1507-4622
Krejci, Radovan
Zieger, Paul
Virtanen, Annele
Riipinen, Ilona
Mohr, Claudia
author_facet Gramlich, Yvette
Siegel, Karolina
Haslett, Sophie L.
Cremer, Roxana S.
Lunder, Chris
Kommula, Snehitha M.
Buchholz, Angela
Yttri, Karl Espen
Chen, Gang
id_orcid:0 000-0002-1507-4622
Krejci, Radovan
Zieger, Paul
Virtanen, Annele
Riipinen, Ilona
Mohr, Claudia
author_sort Gramlich, Yvette
collection ETH Zürich Research Collection
description Emissions from biomass burning (BB) occurring at midlatitudes can reach the Arctic, where they influence the remote aerosol population. By using measurements of levoglucosan and black carbon, we identify seven BB events reaching Svalbard in 2020. We find that most of the BB events are significantly different to the rest of the year (nonevents) for most of the chemical and physical properties. Aerosol mass and number concentrations are enhanced by up to 1 order of magnitude during the BB events. During BB events, the submicrometer aerosol bulk composition changes from an organic- and sulfate-dominated regime to a clearly organic-dominated regime. This results in a significantly lower hygroscopicity parameter κ for BB aerosol (0.4 ± 0.2) compared to nonevents (0.5 ± 0.2), calculated from the nonrefractory aerosol composition. The organic fraction in the BB aerosol showed no significant difference for the O:C ratios (0.9 ± 0.3) compared to the year (0.9 ± 0.6). Accumulation mode particles were present during all BB events, while in the summer an additional Aitken mode was observed, indicating a mixture of the advected air mass with locally produced particles. BB tracers (vanillic, homovanillic, and hydroxybenzoic acid, nitrophenol, methylnitrophenol, and nitrocatechol) were significantly higher when air mass back trajectories passed over active fire regions in Eastern Europe, indicating agricultural and wildfires as sources. Our results suggest that the impact of BB on the Arctic aerosol depends on the season in which they occur, and agricultural and wildfires from Eastern Europe have the potential to disturb the background conditions the most. ISSN:2472-3452
format Article in Journal/Newspaper
genre Arctic
black carbon
Svalbard
genre_facet Arctic
black carbon
Svalbard
geographic Arctic
Svalbard
Aitken
geographic_facet Arctic
Svalbard
Aitken
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institution Open Polar
language English
long_lat ENVELOPE(-44.516,-44.516,-60.733,-60.733)
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op_doi https://doi.org/20.500.11850/66961610.3929/ethz-b-00066961610.1021/acsearthspacechem.3c00187
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1021/acsearthspacechem.3c00187
info:eu-repo/semantics/altIdentifier/wos/001197358000001
info:eu-repo/grantAgreement/EC/H2020/821205
http://hdl.handle.net/20.500.11850/669616
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_source ACS Earth and Space Chemistry, 8 (5)
publishDate 2024
publisher American Chemical Society
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spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/669616 2025-03-30T15:02:56+00:00 Impact of Biomass Burning on Arctic Aerosol Composition Gramlich, Yvette Siegel, Karolina Haslett, Sophie L. Cremer, Roxana S. Lunder, Chris Kommula, Snehitha M. Buchholz, Angela Yttri, Karl Espen Chen, Gang id_orcid:0 000-0002-1507-4622 Krejci, Radovan Zieger, Paul Virtanen, Annele Riipinen, Ilona Mohr, Claudia 2024-05-16 application/application/pdf https://hdl.handle.net/20.500.11850/669616 https://doi.org/10.3929/ethz-b-000669616 en eng American Chemical Society info:eu-repo/semantics/altIdentifier/doi/10.1021/acsearthspacechem.3c00187 info:eu-repo/semantics/altIdentifier/wos/001197358000001 info:eu-repo/grantAgreement/EC/H2020/821205 http://hdl.handle.net/20.500.11850/669616 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International ACS Earth and Space Chemistry, 8 (5) Arctic aerosol Zeppelin Observatory FIGAERO-CIMS aerosol chemical composition biomass burning agricultural fires info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2024 ftethz https://doi.org/20.500.11850/66961610.3929/ethz-b-00066961610.1021/acsearthspacechem.3c00187 2025-03-05T22:09:15Z Emissions from biomass burning (BB) occurring at midlatitudes can reach the Arctic, where they influence the remote aerosol population. By using measurements of levoglucosan and black carbon, we identify seven BB events reaching Svalbard in 2020. We find that most of the BB events are significantly different to the rest of the year (nonevents) for most of the chemical and physical properties. Aerosol mass and number concentrations are enhanced by up to 1 order of magnitude during the BB events. During BB events, the submicrometer aerosol bulk composition changes from an organic- and sulfate-dominated regime to a clearly organic-dominated regime. This results in a significantly lower hygroscopicity parameter κ for BB aerosol (0.4 ± 0.2) compared to nonevents (0.5 ± 0.2), calculated from the nonrefractory aerosol composition. The organic fraction in the BB aerosol showed no significant difference for the O:C ratios (0.9 ± 0.3) compared to the year (0.9 ± 0.6). Accumulation mode particles were present during all BB events, while in the summer an additional Aitken mode was observed, indicating a mixture of the advected air mass with locally produced particles. BB tracers (vanillic, homovanillic, and hydroxybenzoic acid, nitrophenol, methylnitrophenol, and nitrocatechol) were significantly higher when air mass back trajectories passed over active fire regions in Eastern Europe, indicating agricultural and wildfires as sources. Our results suggest that the impact of BB on the Arctic aerosol depends on the season in which they occur, and agricultural and wildfires from Eastern Europe have the potential to disturb the background conditions the most. ISSN:2472-3452 Article in Journal/Newspaper Arctic black carbon Svalbard ETH Zürich Research Collection Arctic Svalbard Aitken ENVELOPE(-44.516,-44.516,-60.733,-60.733)
spellingShingle Arctic aerosol
Zeppelin Observatory
FIGAERO-CIMS
aerosol chemical composition
biomass burning
agricultural fires
Gramlich, Yvette
Siegel, Karolina
Haslett, Sophie L.
Cremer, Roxana S.
Lunder, Chris
Kommula, Snehitha M.
Buchholz, Angela
Yttri, Karl Espen
Chen, Gang
id_orcid:0 000-0002-1507-4622
Krejci, Radovan
Zieger, Paul
Virtanen, Annele
Riipinen, Ilona
Mohr, Claudia
Impact of Biomass Burning on Arctic Aerosol Composition
title Impact of Biomass Burning on Arctic Aerosol Composition
title_full Impact of Biomass Burning on Arctic Aerosol Composition
title_fullStr Impact of Biomass Burning on Arctic Aerosol Composition
title_full_unstemmed Impact of Biomass Burning on Arctic Aerosol Composition
title_short Impact of Biomass Burning on Arctic Aerosol Composition
title_sort impact of biomass burning on arctic aerosol composition
topic Arctic aerosol
Zeppelin Observatory
FIGAERO-CIMS
aerosol chemical composition
biomass burning
agricultural fires
topic_facet Arctic aerosol
Zeppelin Observatory
FIGAERO-CIMS
aerosol chemical composition
biomass burning
agricultural fires
url https://hdl.handle.net/20.500.11850/669616
https://doi.org/10.3929/ethz-b-000669616