Atmospheric Dry Deposition of Water-Soluble Nitrogen to the Subarctic Western North Pacific Ocean during Summer

To estimate dry deposition flux of atmospheric water-soluble nitrogen (N), including ammonium (NH4+), nitrate (NO3−), and water-soluble organic nitrogen (WSON), aerosol samples were collected over the subarctic western North Pacific Ocean in the summer of 2016 aboard the Korean icebreaker IBR/V Arao...

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Published in:Atmosphere
Main Authors: Jinyoung Jung, Byeol Han, Blanca Rodriguez, Yuzo Miyazaki, Hyun Young Chung, Kitae Kim, Jung-Ok Choi, Keyhong Park, II-Nam Kim, Saewung Kim, Eun Jin Yang, Sung-Ho Kang
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Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
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Online Access:https://doi.org/10.3390/atmos10070351
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spelling ftmdpi:oai:mdpi.com:/2073-4433/10/7/351/ 2023-08-20T04:10:02+02:00 Atmospheric Dry Deposition of Water-Soluble Nitrogen to the Subarctic Western North Pacific Ocean during Summer Jinyoung Jung Byeol Han Blanca Rodriguez Yuzo Miyazaki Hyun Young Chung Kitae Kim Jung-Ok Choi Keyhong Park II-Nam Kim Saewung Kim Eun Jin Yang Sung-Ho Kang agris 2019-06-26 application/pdf https://doi.org/10.3390/atmos10070351 EN eng Multidisciplinary Digital Publishing Institute Biosphere/Hydrosphere/Land–Atmosphere Interactions https://dx.doi.org/10.3390/atmos10070351 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 10; Issue 7; Pages: 351 ammonium nitrate water-soluble organic nitrogen influence of sea fog on atmospheric nitrogen atmospheric nitrogen deposition subarctic western North Pacific Ocean Text 2019 ftmdpi https://doi.org/10.3390/atmos10070351 2023-07-31T22:23:17Z To estimate dry deposition flux of atmospheric water-soluble nitrogen (N), including ammonium (NH4+), nitrate (NO3−), and water-soluble organic nitrogen (WSON), aerosol samples were collected over the subarctic western North Pacific Ocean in the summer of 2016 aboard the Korean icebreaker IBR/V Araon. During the cruise, concentrations of NH4+, NO3−, and WSON in bulk (fine + coarse) aerosols ranged from 0.768 to 25.3, 0.199 to 5.94, and 0.116 to 14.7 nmol m−3, respectively. Contributions of NH4+, NO3−, and WSON to total water-soluble N represented ~74%, ~17%, and ~9%, respectively. Water-soluble N concentrations showed a strong gradient from the East Asian continent to the subarctic western North Pacific Ocean, indicating that water-soluble N species were mainly derived from anthropogenic or terrestrial sources. During sea fog events, coarse mode NO3− was likely to be scavenged more efficiently by fog droplets than fine mode NO3−; besides, WSON was detected only in fine mode, suggesting that there may have been a significant influence of sea fog on WSON, such as the photochemical conversion of WSON into inorganic N. Mean dry deposition flux for water-soluble total N (6.3 ± 9.4 µmol m−2 d−1) over the subarctic western North Pacific Ocean was estimated to support a minimum carbon uptake of 42 ± 62 µmol C m−2d−1 by using the Redfield C/N ratio of 6.625. Text Subarctic MDPI Open Access Publishing Pacific Atmosphere 10 7 351
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic ammonium
nitrate
water-soluble organic nitrogen
influence of sea fog on atmospheric nitrogen
atmospheric nitrogen deposition
subarctic western North Pacific Ocean
spellingShingle ammonium
nitrate
water-soluble organic nitrogen
influence of sea fog on atmospheric nitrogen
atmospheric nitrogen deposition
subarctic western North Pacific Ocean
Jinyoung Jung
Byeol Han
Blanca Rodriguez
Yuzo Miyazaki
Hyun Young Chung
Kitae Kim
Jung-Ok Choi
Keyhong Park
II-Nam Kim
Saewung Kim
Eun Jin Yang
Sung-Ho Kang
Atmospheric Dry Deposition of Water-Soluble Nitrogen to the Subarctic Western North Pacific Ocean during Summer
topic_facet ammonium
nitrate
water-soluble organic nitrogen
influence of sea fog on atmospheric nitrogen
atmospheric nitrogen deposition
subarctic western North Pacific Ocean
description To estimate dry deposition flux of atmospheric water-soluble nitrogen (N), including ammonium (NH4+), nitrate (NO3−), and water-soluble organic nitrogen (WSON), aerosol samples were collected over the subarctic western North Pacific Ocean in the summer of 2016 aboard the Korean icebreaker IBR/V Araon. During the cruise, concentrations of NH4+, NO3−, and WSON in bulk (fine + coarse) aerosols ranged from 0.768 to 25.3, 0.199 to 5.94, and 0.116 to 14.7 nmol m−3, respectively. Contributions of NH4+, NO3−, and WSON to total water-soluble N represented ~74%, ~17%, and ~9%, respectively. Water-soluble N concentrations showed a strong gradient from the East Asian continent to the subarctic western North Pacific Ocean, indicating that water-soluble N species were mainly derived from anthropogenic or terrestrial sources. During sea fog events, coarse mode NO3− was likely to be scavenged more efficiently by fog droplets than fine mode NO3−; besides, WSON was detected only in fine mode, suggesting that there may have been a significant influence of sea fog on WSON, such as the photochemical conversion of WSON into inorganic N. Mean dry deposition flux for water-soluble total N (6.3 ± 9.4 µmol m−2 d−1) over the subarctic western North Pacific Ocean was estimated to support a minimum carbon uptake of 42 ± 62 µmol C m−2d−1 by using the Redfield C/N ratio of 6.625.
format Text
author Jinyoung Jung
Byeol Han
Blanca Rodriguez
Yuzo Miyazaki
Hyun Young Chung
Kitae Kim
Jung-Ok Choi
Keyhong Park
II-Nam Kim
Saewung Kim
Eun Jin Yang
Sung-Ho Kang
author_facet Jinyoung Jung
Byeol Han
Blanca Rodriguez
Yuzo Miyazaki
Hyun Young Chung
Kitae Kim
Jung-Ok Choi
Keyhong Park
II-Nam Kim
Saewung Kim
Eun Jin Yang
Sung-Ho Kang
author_sort Jinyoung Jung
title Atmospheric Dry Deposition of Water-Soluble Nitrogen to the Subarctic Western North Pacific Ocean during Summer
title_short Atmospheric Dry Deposition of Water-Soluble Nitrogen to the Subarctic Western North Pacific Ocean during Summer
title_full Atmospheric Dry Deposition of Water-Soluble Nitrogen to the Subarctic Western North Pacific Ocean during Summer
title_fullStr Atmospheric Dry Deposition of Water-Soluble Nitrogen to the Subarctic Western North Pacific Ocean during Summer
title_full_unstemmed Atmospheric Dry Deposition of Water-Soluble Nitrogen to the Subarctic Western North Pacific Ocean during Summer
title_sort atmospheric dry deposition of water-soluble nitrogen to the subarctic western north pacific ocean during summer
publisher Multidisciplinary Digital Publishing Institute
publishDate 2019
url https://doi.org/10.3390/atmos10070351
op_coverage agris
geographic Pacific
geographic_facet Pacific
genre Subarctic
genre_facet Subarctic
op_source Atmosphere; Volume 10; Issue 7; Pages: 351
op_relation Biosphere/Hydrosphere/Land–Atmosphere Interactions
https://dx.doi.org/10.3390/atmos10070351
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos10070351
container_title Atmosphere
container_volume 10
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