Characteristics and sources of fluorescent aerosols in the central Arctic Ocean

International audience The Arctic is sensitive to cloud radiative forcing. Due to the limited number of aerosols present throughout much of the year, cloud formation is susceptible to the presence of cloud condensation nuclei and ice nucleating particles (INPs). Primary biological aerosol particles...

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Published in:Elem Sci Anth
Main Authors: Beck, Ivo, Moallemi, Alireza, Heutte, Benjamin, Pernov, Jakob, Boyd, Bergner, Nora, Rolo, Margarida, Quéléver, Lauriane, L J, Laurila, Tiia, Boyer, Matthew, Jokinen, Tuija, Angot, Hélène, Hoppe, Clara, J M, Müller, Oliver, Creamean, Jessie, Frey, Markus, M, Freitas, Gabriel, Zinke, Julika, Salter, Matt, Zieger, Paul, Mirrielees, Jessica, A, Kempf, Hailey, E, Ault, Andrew, P, Pratt, Kerri, A, Gysel-Beer, Martin, Henning, Silvia, Tatzelt, Christian, Schmale, Julia
Other Authors: Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), Ecole Polytechnique Fédérale de Lausanne (EPFL)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2024
Subjects:
Online Access:https://hal.science/hal-04597406
https://hal.science/hal-04597406/document
https://hal.science/hal-04597406/file/Beck%20et%20al.%20-%202024%20-%20Characteristics%20and%20sources%20of%20fluorescent%20aerosol.pdf
https://doi.org/10.1525/elementa.2023.00125
id ftinsu:oai:HAL:hal-04597406v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic Arctic
Fluorescent aerosol
Primary biological aerosol particles
MOSAiC expedition
Air-sea-iceexchange
Ice nucleating particles
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle Arctic
Fluorescent aerosol
Primary biological aerosol particles
MOSAiC expedition
Air-sea-iceexchange
Ice nucleating particles
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Beck, Ivo
Moallemi, Alireza
Heutte, Benjamin
Pernov, Jakob, Boyd
Bergner, Nora
Rolo, Margarida
Quéléver, Lauriane, L J
Laurila, Tiia
Boyer, Matthew
Jokinen, Tuija
Angot, Hélène
Hoppe, Clara, J M
Müller, Oliver
Creamean, Jessie
Frey, Markus, M
Freitas, Gabriel
Zinke, Julika
Salter, Matt
Zieger, Paul
Mirrielees, Jessica, A
Kempf, Hailey, E
Ault, Andrew, P
Pratt, Kerri, A
Gysel-Beer, Martin
Henning, Silvia
Tatzelt, Christian
Schmale, Julia
Characteristics and sources of fluorescent aerosols in the central Arctic Ocean
topic_facet Arctic
Fluorescent aerosol
Primary biological aerosol particles
MOSAiC expedition
Air-sea-iceexchange
Ice nucleating particles
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
description International audience The Arctic is sensitive to cloud radiative forcing. Due to the limited number of aerosols present throughout much of the year, cloud formation is susceptible to the presence of cloud condensation nuclei and ice nucleating particles (INPs). Primary biological aerosol particles (PBAP) contribute to INPs and can impact cloud phase, lifetime, and radiative properties. We present yearlong observations of hyperfluorescent aerosols (HFA), tracers for PBAP, conducted with a Wideband Integrated Bioaerosol Sensor, New Electronics Option during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition (October 2019–September 2020) in the central Arctic. We investigate the influence of potential anthropogenic and natural sources on the characteristics of the HFA and relate our measurements to INP observations during MOSAiC. Anthropogenic sources influenced HFA during the Arctic haze period. But surprisingly, we also found sporadic “bursts” of HFA with the characteristics of PBAP during this time, albeit with unclear origin. The characteristics of HFA between May and August 2020 and in October 2019 indicate a strong contribution of PBAP to HFA. Notably from May to August, PBAP coincided with the presence of INPs nucleating at elevated temperatures, that is, >−9°C, suggesting that HFA contributed to the “warm INP” concentration. The air mass residence time and area between May and August and in October were dominated by the open ocean and sea ice, pointing toward PBAP sources from within the Arctic Ocean. As the central Arctic changes drastically due to climate warming with expected implications on aerosol–cloud interactions, we recommend targeted observations of PBAP that reveal their nature (e.g., bacteria, diatoms, fungal spores) in the atmosphere and in relevant surface sources, such as the sea ice, snow on sea ice, melt ponds, leads, and open water, to gain further insights into the relevant source processes and how they might change in the future.
author2 Institut des Géosciences de l’Environnement (IGE)
Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )
Université Grenoble Alpes (UGA)
Ecole Polytechnique Fédérale de Lausanne (EPFL)
format Article in Journal/Newspaper
author Beck, Ivo
Moallemi, Alireza
Heutte, Benjamin
Pernov, Jakob, Boyd
Bergner, Nora
Rolo, Margarida
Quéléver, Lauriane, L J
Laurila, Tiia
Boyer, Matthew
Jokinen, Tuija
Angot, Hélène
Hoppe, Clara, J M
Müller, Oliver
Creamean, Jessie
Frey, Markus, M
Freitas, Gabriel
Zinke, Julika
Salter, Matt
Zieger, Paul
Mirrielees, Jessica, A
Kempf, Hailey, E
Ault, Andrew, P
Pratt, Kerri, A
Gysel-Beer, Martin
Henning, Silvia
Tatzelt, Christian
Schmale, Julia
author_facet Beck, Ivo
Moallemi, Alireza
Heutte, Benjamin
Pernov, Jakob, Boyd
Bergner, Nora
Rolo, Margarida
Quéléver, Lauriane, L J
Laurila, Tiia
Boyer, Matthew
Jokinen, Tuija
Angot, Hélène
Hoppe, Clara, J M
Müller, Oliver
Creamean, Jessie
Frey, Markus, M
Freitas, Gabriel
Zinke, Julika
Salter, Matt
Zieger, Paul
Mirrielees, Jessica, A
Kempf, Hailey, E
Ault, Andrew, P
Pratt, Kerri, A
Gysel-Beer, Martin
Henning, Silvia
Tatzelt, Christian
Schmale, Julia
author_sort Beck, Ivo
title Characteristics and sources of fluorescent aerosols in the central Arctic Ocean
title_short Characteristics and sources of fluorescent aerosols in the central Arctic Ocean
title_full Characteristics and sources of fluorescent aerosols in the central Arctic Ocean
title_fullStr Characteristics and sources of fluorescent aerosols in the central Arctic Ocean
title_full_unstemmed Characteristics and sources of fluorescent aerosols in the central Arctic Ocean
title_sort characteristics and sources of fluorescent aerosols in the central arctic ocean
publisher HAL CCSD
publishDate 2024
url https://hal.science/hal-04597406
https://hal.science/hal-04597406/document
https://hal.science/hal-04597406/file/Beck%20et%20al.%20-%202024%20-%20Characteristics%20and%20sources%20of%20fluorescent%20aerosol.pdf
https://doi.org/10.1525/elementa.2023.00125
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_source EISSN: 2325-1026
Elementa: Science of the Anthropocene
https://hal.science/hal-04597406
Elementa: Science of the Anthropocene, 2024, 12 (1), pp.00125. ⟨10.1525/elementa.2023.00125⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1525/elementa.2023.00125
hal-04597406
https://hal.science/hal-04597406
https://hal.science/hal-04597406/document
https://hal.science/hal-04597406/file/Beck%20et%20al.%20-%202024%20-%20Characteristics%20and%20sources%20of%20fluorescent%20aerosol.pdf
doi:10.1525/elementa.2023.00125
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1525/elementa.2023.00125
container_title Elem Sci Anth
container_volume 12
container_issue 1
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spelling ftinsu:oai:HAL:hal-04597406v1 2024-06-23T07:49:21+00:00 Characteristics and sources of fluorescent aerosols in the central Arctic Ocean Beck, Ivo Moallemi, Alireza Heutte, Benjamin Pernov, Jakob, Boyd Bergner, Nora Rolo, Margarida Quéléver, Lauriane, L J Laurila, Tiia Boyer, Matthew Jokinen, Tuija Angot, Hélène Hoppe, Clara, J M Müller, Oliver Creamean, Jessie Frey, Markus, M Freitas, Gabriel Zinke, Julika Salter, Matt Zieger, Paul Mirrielees, Jessica, A Kempf, Hailey, E Ault, Andrew, P Pratt, Kerri, A Gysel-Beer, Martin Henning, Silvia Tatzelt, Christian Schmale, Julia Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) Ecole Polytechnique Fédérale de Lausanne (EPFL) 2024 https://hal.science/hal-04597406 https://hal.science/hal-04597406/document https://hal.science/hal-04597406/file/Beck%20et%20al.%20-%202024%20-%20Characteristics%20and%20sources%20of%20fluorescent%20aerosol.pdf https://doi.org/10.1525/elementa.2023.00125 en eng HAL CCSD University of California Press info:eu-repo/semantics/altIdentifier/doi/10.1525/elementa.2023.00125 hal-04597406 https://hal.science/hal-04597406 https://hal.science/hal-04597406/document https://hal.science/hal-04597406/file/Beck%20et%20al.%20-%202024%20-%20Characteristics%20and%20sources%20of%20fluorescent%20aerosol.pdf doi:10.1525/elementa.2023.00125 info:eu-repo/semantics/OpenAccess EISSN: 2325-1026 Elementa: Science of the Anthropocene https://hal.science/hal-04597406 Elementa: Science of the Anthropocene, 2024, 12 (1), pp.00125. ⟨10.1525/elementa.2023.00125⟩ Arctic Fluorescent aerosol Primary biological aerosol particles MOSAiC expedition Air-sea-iceexchange Ice nucleating particles [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2024 ftinsu https://doi.org/10.1525/elementa.2023.00125 2024-06-06T00:00:14Z International audience The Arctic is sensitive to cloud radiative forcing. Due to the limited number of aerosols present throughout much of the year, cloud formation is susceptible to the presence of cloud condensation nuclei and ice nucleating particles (INPs). Primary biological aerosol particles (PBAP) contribute to INPs and can impact cloud phase, lifetime, and radiative properties. We present yearlong observations of hyperfluorescent aerosols (HFA), tracers for PBAP, conducted with a Wideband Integrated Bioaerosol Sensor, New Electronics Option during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition (October 2019–September 2020) in the central Arctic. We investigate the influence of potential anthropogenic and natural sources on the characteristics of the HFA and relate our measurements to INP observations during MOSAiC. Anthropogenic sources influenced HFA during the Arctic haze period. But surprisingly, we also found sporadic “bursts” of HFA with the characteristics of PBAP during this time, albeit with unclear origin. The characteristics of HFA between May and August 2020 and in October 2019 indicate a strong contribution of PBAP to HFA. Notably from May to August, PBAP coincided with the presence of INPs nucleating at elevated temperatures, that is, >−9°C, suggesting that HFA contributed to the “warm INP” concentration. The air mass residence time and area between May and August and in October were dominated by the open ocean and sea ice, pointing toward PBAP sources from within the Arctic Ocean. As the central Arctic changes drastically due to climate warming with expected implications on aerosol–cloud interactions, we recommend targeted observations of PBAP that reveal their nature (e.g., bacteria, diatoms, fungal spores) in the atmosphere and in relevant surface sources, such as the sea ice, snow on sea ice, melt ponds, leads, and open water, to gain further insights into the relevant source processes and how they might change in the future. Article in Journal/Newspaper Arctic Arctic Ocean Sea ice Institut national des sciences de l'Univers: HAL-INSU Arctic Arctic Ocean Elem Sci Anth 12 1