A central arctic extreme aerosol event triggered by a warm air-mass intrusion

Warm and moist air-mass intrusions into the Arctic are more frequent than the past decades. Here, the authors show that warm air mass intrusions from northern Eurasia inject record amounts of aerosols into the central Arctic Ocean strongly impacting atmospheric chemistry and cloud properties. Freque...

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Published in:Nature Communications
Main Authors: Dada, Lubna, Angot, Helene, Beck, Ivo, Baccarini, Andrea, Quelever, Lauriane L. J., Boyer, Matthew, Laurila, Tiia, Brasseur, Zoe, Jozef, Gina, de Boer, Gijs, Shupe, Matthew D., Henning, Silvia, Bucci, Silvia, Dütsch, Marina, Stohl, Andreas, Petäjä, Tuukka, Daellenbach, Kaspar R., Jokinen, Tuija, Schmale, Julia
Other Authors: Polar and arctic atmospheric research (PANDA), Institute for Atmospheric and Earth System Research (INAR)
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2022
Subjects:
Online Access:http://hdl.handle.net/10138/351019
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spelling ftunivhelsihelda:oai:helda.helsinki.fi:10138/351019 2024-01-07T09:40:47+01:00 A central arctic extreme aerosol event triggered by a warm air-mass intrusion Dada, Lubna Angot, Helene Beck, Ivo Baccarini, Andrea Quelever, Lauriane L. J. Boyer, Matthew Laurila, Tiia Brasseur, Zoe Jozef, Gina de Boer, Gijs Shupe, Matthew D. Henning, Silvia Bucci, Silvia Dütsch, Marina Stohl, Andreas Petäjä, Tuukka Daellenbach, Kaspar R. Jokinen, Tuija Schmale, Julia Polar and arctic atmospheric research (PANDA) Institute for Atmospheric and Earth System Research (INAR) 2022-11-24T11:15:01Z 15 application/pdf http://hdl.handle.net/10138/351019 eng eng Nature Publishing Group 10.1038/s41467-022-32872-2 This research was funded by the Swiss National Science Foundation (grant 200021_188478) and the Swiss Polar Institute (J.S.). UAS observations and data processing and analysis was supported by the US National Science Foundation (OPP 1805569) and the NOAA Physical Sciences Laboratory (G.B.). European Research Council ERC (GASPARCON-grant no 714621) is acknowledged (L.Q.). This work was supported by the Academy of Finland (project 334514) and the EMME-CARE projectwhich received funding from the European Union's Horizon 2020 Research and Innovation Programme, under grant agreement no. 856612 (T.J.). work was 994 supported by Academy of Finland via project (333397) and Atmosphere and Climate Competence Center (337549) and University of Helsinki ACTRIS-HY (T.P.). The US Department of Energy Atmospheric System Research Program (DE-SC0019251, DESC0021341) is acknowledged for financial support (M.D.S.). Support by the Swiss National Science Foundation Ambizione grant PZPGP2_201992 is acknowledged (K.R.D.). Dada , L , Angot , H , Beck , I , Baccarini , A , Quelever , L L J , Boyer , M , Laurila , T , Brasseur , Z , Jozef , G , de Boer , G , Shupe , M D , Henning , S , Bucci , S , Dütsch , M , Stohl , A , Petäjä , T , Daellenbach , K R , Jokinen , T & Schmale , J 2022 , ' A central arctic extreme aerosol event triggered by a warm air-mass intrusion ' , Nature Communications , vol. 13 , no. 1 , 5290 . https://doi.org/10.1038/s41467-022-32872-2 ORCID: /0000-0002-1881-9044/work/123553097 ORCID: /0000-0003-1105-9043/work/123558448 ORCID: /0000-0001-5387-018X/work/123559031 36075920 85134894407 5d105761-4dca-4474-a984-f33cddfd7dbd http://hdl.handle.net/10138/351019 000852448100011 cc_by openAccess info:eu-repo/semantics/openAccess 114 Physical sciences Article publishedVersion 2022 ftunivhelsihelda 2023-12-14T00:05:30Z Warm and moist air-mass intrusions into the Arctic are more frequent than the past decades. Here, the authors show that warm air mass intrusions from northern Eurasia inject record amounts of aerosols into the central Arctic Ocean strongly impacting atmospheric chemistry and cloud properties. Frequency and intensity of warm and moist air-mass intrusions into the Arctic have increased over the past decades and have been related to sea ice melt. During our year-long expedition in the remote central Arctic Ocean, a record-breaking increase in temperature, moisture and downwelling-longwave radiation was observed in mid-April 2020, during an air-mass intrusion carrying air pollutants from northern Eurasia. The two-day intrusion, caused drastic changes in the aerosol size distribution, chemical composition and particle hygroscopicity. Here we show how the intrusion transformed the Arctic from a remote low-particle environment to an area comparable to a central-European urban setting. Additionally, the intrusion resulted in an explosive increase in cloud condensation nuclei, which can have direct effects on Arctic clouds' radiation, their precipitation patterns, and their lifetime. Thus, unless prompt actions to significantly reduce emissions in the source regions are taken, such intrusion events are expected to continue to affect the Arctic climate. Peer reviewed Article in Journal/Newspaper Arctic Arctic Arctic Ocean Sea ice HELDA – University of Helsinki Open Repository Arctic Arctic Ocean Nature Communications 13 1
institution Open Polar
collection HELDA – University of Helsinki Open Repository
op_collection_id ftunivhelsihelda
language English
topic 114 Physical sciences
spellingShingle 114 Physical sciences
Dada, Lubna
Angot, Helene
Beck, Ivo
Baccarini, Andrea
Quelever, Lauriane L. J.
Boyer, Matthew
Laurila, Tiia
Brasseur, Zoe
Jozef, Gina
de Boer, Gijs
Shupe, Matthew D.
Henning, Silvia
Bucci, Silvia
Dütsch, Marina
Stohl, Andreas
Petäjä, Tuukka
Daellenbach, Kaspar R.
Jokinen, Tuija
Schmale, Julia
A central arctic extreme aerosol event triggered by a warm air-mass intrusion
topic_facet 114 Physical sciences
description Warm and moist air-mass intrusions into the Arctic are more frequent than the past decades. Here, the authors show that warm air mass intrusions from northern Eurasia inject record amounts of aerosols into the central Arctic Ocean strongly impacting atmospheric chemistry and cloud properties. Frequency and intensity of warm and moist air-mass intrusions into the Arctic have increased over the past decades and have been related to sea ice melt. During our year-long expedition in the remote central Arctic Ocean, a record-breaking increase in temperature, moisture and downwelling-longwave radiation was observed in mid-April 2020, during an air-mass intrusion carrying air pollutants from northern Eurasia. The two-day intrusion, caused drastic changes in the aerosol size distribution, chemical composition and particle hygroscopicity. Here we show how the intrusion transformed the Arctic from a remote low-particle environment to an area comparable to a central-European urban setting. Additionally, the intrusion resulted in an explosive increase in cloud condensation nuclei, which can have direct effects on Arctic clouds' radiation, their precipitation patterns, and their lifetime. Thus, unless prompt actions to significantly reduce emissions in the source regions are taken, such intrusion events are expected to continue to affect the Arctic climate. Peer reviewed
author2 Polar and arctic atmospheric research (PANDA)
Institute for Atmospheric and Earth System Research (INAR)
format Article in Journal/Newspaper
author Dada, Lubna
Angot, Helene
Beck, Ivo
Baccarini, Andrea
Quelever, Lauriane L. J.
Boyer, Matthew
Laurila, Tiia
Brasseur, Zoe
Jozef, Gina
de Boer, Gijs
Shupe, Matthew D.
Henning, Silvia
Bucci, Silvia
Dütsch, Marina
Stohl, Andreas
Petäjä, Tuukka
Daellenbach, Kaspar R.
Jokinen, Tuija
Schmale, Julia
author_facet Dada, Lubna
Angot, Helene
Beck, Ivo
Baccarini, Andrea
Quelever, Lauriane L. J.
Boyer, Matthew
Laurila, Tiia
Brasseur, Zoe
Jozef, Gina
de Boer, Gijs
Shupe, Matthew D.
Henning, Silvia
Bucci, Silvia
Dütsch, Marina
Stohl, Andreas
Petäjä, Tuukka
Daellenbach, Kaspar R.
Jokinen, Tuija
Schmale, Julia
author_sort Dada, Lubna
title A central arctic extreme aerosol event triggered by a warm air-mass intrusion
title_short A central arctic extreme aerosol event triggered by a warm air-mass intrusion
title_full A central arctic extreme aerosol event triggered by a warm air-mass intrusion
title_fullStr A central arctic extreme aerosol event triggered by a warm air-mass intrusion
title_full_unstemmed A central arctic extreme aerosol event triggered by a warm air-mass intrusion
title_sort central arctic extreme aerosol event triggered by a warm air-mass intrusion
publisher Nature Publishing Group
publishDate 2022
url http://hdl.handle.net/10138/351019
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic
Arctic Ocean
Sea ice
op_relation 10.1038/s41467-022-32872-2
This research was funded by the Swiss National Science Foundation (grant 200021_188478) and the Swiss Polar Institute (J.S.). UAS observations and data processing and analysis was supported by the US National Science Foundation (OPP 1805569) and the NOAA Physical Sciences Laboratory (G.B.). European Research Council ERC (GASPARCON-grant no 714621) is acknowledged (L.Q.). This work was supported by the Academy of Finland (project 334514) and the EMME-CARE projectwhich received funding from the European Union's Horizon 2020 Research and Innovation Programme, under grant agreement no. 856612 (T.J.). work was 994 supported by Academy of Finland via project (333397) and Atmosphere and Climate Competence Center (337549) and University of Helsinki ACTRIS-HY (T.P.). The US Department of Energy Atmospheric System Research Program (DE-SC0019251, DESC0021341) is acknowledged for financial support (M.D.S.). Support by the Swiss National Science Foundation Ambizione grant PZPGP2_201992 is acknowledged (K.R.D.).
Dada , L , Angot , H , Beck , I , Baccarini , A , Quelever , L L J , Boyer , M , Laurila , T , Brasseur , Z , Jozef , G , de Boer , G , Shupe , M D , Henning , S , Bucci , S , Dütsch , M , Stohl , A , Petäjä , T , Daellenbach , K R , Jokinen , T & Schmale , J 2022 , ' A central arctic extreme aerosol event triggered by a warm air-mass intrusion ' , Nature Communications , vol. 13 , no. 1 , 5290 . https://doi.org/10.1038/s41467-022-32872-2
ORCID: /0000-0002-1881-9044/work/123553097
ORCID: /0000-0003-1105-9043/work/123558448
ORCID: /0000-0001-5387-018X/work/123559031
36075920
85134894407
5d105761-4dca-4474-a984-f33cddfd7dbd
http://hdl.handle.net/10138/351019
000852448100011
op_rights cc_by
openAccess
info:eu-repo/semantics/openAccess
container_title Nature Communications
container_volume 13
container_issue 1
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