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

• 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
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2019
• Subjects: ammonium; nitrate; water-soluble organic nitrogen; influence of sea fog on atmospheric nitrogen; atmospheric nitrogen deposition; subarctic western North Pacific Ocean; Meteorology. Climatology; QC851-999; Pacific; Subarctic
• Online Access: https://doi.org/10.3390/atmos10070351; https://doaj.org/article/0d61b853bdc4417c861c14b0e304b5c9

To estimate dry deposition flux of atmospheric water-soluble nitrogen (N), including ammonium (NH 4 + ), nitrate (NO 3 − ), 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 NH 4 + , NO 3 − , 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 NH 4 + , NO 3 − , 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 NO 3 − was likely to be scavenged more efficiently by fog droplets than fine mode NO 3 − 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 −2 d −1 by using the Redfield C/N ratio of 6.625.