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...
Main Authors: | , , , , , , , , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Chemical Society
2024
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11850/669616 https://doi.org/10.3929/ethz-b-000669616 |
_version_ | 1828053326879522816 |
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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 |
id | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/669616 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-44.516,-44.516,-60.733,-60.733) |
op_collection_id | ftethz |
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 |
record_format | openpolar |
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 |