New particle formation events observed at the King Sejong Station, Antarctic Peninsula - Part 2: Link with the oceanic biological activities
Abstract. Marine biota is an important source of atmospheric aerosol particles in the remote marine atmosphere. However, the relationship between new particle formation and marine biota is poorly quantified. Long-term observations (from 2009 to 2016) of the physical properties of atmospheric aerosol...
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ftopenaccessrep:oai:zenodo.org:68246 2024-09-15T17:47:39+00:00 New particle formation events observed at the King Sejong Station, Antarctic Peninsula - Part 2: Link with the oceanic biological activities Eunho Jang Ki-Tae Park Young Jun Yoon Tae-Wook Kim Sang-Bum Hong Silvia Becagli Rita Traversi Jaeseok Kim Yeontae Gim 2019-06-06 https://www.openaccessrepository.it/record/68246 https://doi.org/10.5194/acp-19-7595-2019 eng eng url:https://www.openaccessrepository.it/communities/itmirror https://www.openaccessrepository.it/record/68246 doi:10.5194/acp-19-7595-2019 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/ Atmospheric Science info:eu-repo/semantics/article publication-article 2019 ftopenaccessrep https://doi.org/10.5194/acp-19-7595-2019 2024-07-29T03:27:38Z Abstract. Marine biota is an important source of atmospheric aerosol particles in the remote marine atmosphere. However, the relationship between new particle formation and marine biota is poorly quantified. Long-term observations (from 2009 to 2016) of the physical properties of atmospheric aerosol particles measured at the Antarctic Peninsula (King Sejong Station; 62.2∘ S, 58.8∘ W) and satellite-derived estimates of the biological characteristics were analyzed to identify the link between new particle formation and marine biota. New particle formation events in the Antarctic atmosphere showed distinct seasonal variations, with the highest values occurring when the air mass originated from the ocean domain during the productive austral summer (December, January and February). Interestingly, new particle formation events were more frequent in the air masses that originated from the Bellingshausen Sea than in those that originated from the Weddell Sea. The monthly mean number concentration of nanoparticles (2.5–10 nm in diameter) was >2-fold higher when the air masses passed over the Bellingshausen Sea than the Weddell Sea, whereas the biomass of phytoplankton in the Weddell Sea was more than ∼70 % higher than that of the Bellingshausen Sea during the austral summer period. Dimethyl sulfide (DMS) is of marine origin and its oxidative products are known to be one of the major components in the formation of new particles. Both satellite-derived estimates of the biological characteristics (dimethylsulfoniopropionate, DMSP; precursor of DMS) and phytoplankton taxonomic composition and in situ methanesulfonic acid (84 daily measurements during the summer period in 2013 and 2014) analysis revealed that DMS(P)-rich phytoplankton were more dominant in the Bellingshausen Sea than in the Weddell Sea. Furthermore, the number concentration of nanoparticles was positively correlated with the biomass of phytoplankton during the period when DMS(P)-rich phytoplankton predominate. These results indicate that ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Bellingshausen Sea Weddell Sea Istituto Nazionale di Fisica Nucleare (INFN): Open Access Repository Atmospheric Chemistry and Physics 19 11 7595 7608 |
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Open Polar |
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Istituto Nazionale di Fisica Nucleare (INFN): Open Access Repository |
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language |
English |
topic |
Atmospheric Science |
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Atmospheric Science Eunho Jang Ki-Tae Park Young Jun Yoon Tae-Wook Kim Sang-Bum Hong Silvia Becagli Rita Traversi Jaeseok Kim Yeontae Gim New particle formation events observed at the King Sejong Station, Antarctic Peninsula - Part 2: Link with the oceanic biological activities |
topic_facet |
Atmospheric Science |
description |
Abstract. Marine biota is an important source of atmospheric aerosol particles in the remote marine atmosphere. However, the relationship between new particle formation and marine biota is poorly quantified. Long-term observations (from 2009 to 2016) of the physical properties of atmospheric aerosol particles measured at the Antarctic Peninsula (King Sejong Station; 62.2∘ S, 58.8∘ W) and satellite-derived estimates of the biological characteristics were analyzed to identify the link between new particle formation and marine biota. New particle formation events in the Antarctic atmosphere showed distinct seasonal variations, with the highest values occurring when the air mass originated from the ocean domain during the productive austral summer (December, January and February). Interestingly, new particle formation events were more frequent in the air masses that originated from the Bellingshausen Sea than in those that originated from the Weddell Sea. The monthly mean number concentration of nanoparticles (2.5–10 nm in diameter) was >2-fold higher when the air masses passed over the Bellingshausen Sea than the Weddell Sea, whereas the biomass of phytoplankton in the Weddell Sea was more than ∼70 % higher than that of the Bellingshausen Sea during the austral summer period. Dimethyl sulfide (DMS) is of marine origin and its oxidative products are known to be one of the major components in the formation of new particles. Both satellite-derived estimates of the biological characteristics (dimethylsulfoniopropionate, DMSP; precursor of DMS) and phytoplankton taxonomic composition and in situ methanesulfonic acid (84 daily measurements during the summer period in 2013 and 2014) analysis revealed that DMS(P)-rich phytoplankton were more dominant in the Bellingshausen Sea than in the Weddell Sea. Furthermore, the number concentration of nanoparticles was positively correlated with the biomass of phytoplankton during the period when DMS(P)-rich phytoplankton predominate. These results indicate that ... |
format |
Article in Journal/Newspaper |
author |
Eunho Jang Ki-Tae Park Young Jun Yoon Tae-Wook Kim Sang-Bum Hong Silvia Becagli Rita Traversi Jaeseok Kim Yeontae Gim |
author_facet |
Eunho Jang Ki-Tae Park Young Jun Yoon Tae-Wook Kim Sang-Bum Hong Silvia Becagli Rita Traversi Jaeseok Kim Yeontae Gim |
author_sort |
Eunho Jang |
title |
New particle formation events observed at the King Sejong Station, Antarctic Peninsula - Part 2: Link with the oceanic biological activities |
title_short |
New particle formation events observed at the King Sejong Station, Antarctic Peninsula - Part 2: Link with the oceanic biological activities |
title_full |
New particle formation events observed at the King Sejong Station, Antarctic Peninsula - Part 2: Link with the oceanic biological activities |
title_fullStr |
New particle formation events observed at the King Sejong Station, Antarctic Peninsula - Part 2: Link with the oceanic biological activities |
title_full_unstemmed |
New particle formation events observed at the King Sejong Station, Antarctic Peninsula - Part 2: Link with the oceanic biological activities |
title_sort |
new particle formation events observed at the king sejong station, antarctic peninsula - part 2: link with the oceanic biological activities |
publishDate |
2019 |
url |
https://www.openaccessrepository.it/record/68246 https://doi.org/10.5194/acp-19-7595-2019 |
genre |
Antarc* Antarctic Antarctic Peninsula Bellingshausen Sea Weddell Sea |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Bellingshausen Sea Weddell Sea |
op_relation |
url:https://www.openaccessrepository.it/communities/itmirror https://www.openaccessrepository.it/record/68246 doi:10.5194/acp-19-7595-2019 |
op_rights |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.5194/acp-19-7595-2019 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
19 |
container_issue |
11 |
container_start_page |
7595 |
op_container_end_page |
7608 |
_version_ |
1810497115611201536 |