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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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 |
container_issue |
7 |
container_start_page |
351 |
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1774723916280889344 |