Mixing state and distribution of iodine-containing particles in Arctic Ocean during summertime
10 pags., 6 figs., 1 tab. Iodine chemistry plays a key role in ozone destruction and new aerosol formation in the marine boundary layer (MBL), especially in polar regions. We investigated iodine-containing particles (0.2-2 μm) in the Arctic Ocean using a ship-based single particle aerosol mass spect...
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ftcsic:oai:digital.csic.es:10261/280314 2024-02-11T09:57:06+01:00 Mixing state and distribution of iodine-containing particles in Arctic Ocean during summertime Wang, Longquan Yan, Jingpei Saiz-Lopez, A. Jiang, Bei Yue, Fange Yu, Xiawei Xie, Zhouqing National Natural Science Foundation of China 2022-04-04 http://hdl.handle.net/10261/280314 https://doi.org/10.1016/j.scitotenv.2022.155030 https://doi.org/10.13039/501100001809 unknown Elsevier Postprint http://dx.doi.org/10.1016/j.scitotenv.2022.155030 Sí doi:10.1016/j.scitotenv.2022.155030 issn: 1879-1026 Science of the Total Environment 834: 155030 (2022) http://hdl.handle.net/10261/280314 http://dx.doi.org/10.13039/501100001809 embargo_20240404 Arctic Ocean Iodine chemistry Single particle Sea ice Diurnal trends artículo 2022 ftcsic https://doi.org/10.1016/j.scitotenv.2022.15503010.13039/501100001809 2024-01-16T11:29:34Z 10 pags., 6 figs., 1 tab. Iodine chemistry plays a key role in ozone destruction and new aerosol formation in the marine boundary layer (MBL), especially in polar regions. We investigated iodine-containing particles (0.2-2 μm) in the Arctic Ocean using a ship-based single particle aerosol mass spectrometer from July to August 2017. Seven main particle types were identified: dust, biomass combustion particles, sea salt, organic S, aromatics, hydrocarbon-like compounds, and amines. The number fraction of iodine-containing particles was higher inside the Arctic Circle (>65°N) than outside (55–65°N). According to the air mass back trajectories, the latitudinal distribution of iodine-containing particles can be mainly attributed to iodine emissions from the sea ice edge region. Diurnal trends were found, especially during the second half of cruise, with peak iodine-containing particle number fractions during low-light conditions and relatively low number fractions at midday. These results imply that solar radiation plays a significant role in modulating particulate iodine in the Arctic atmosphere. This work was supported by the National Natural Science Foundation of China (NSFC) (41941014). We thank China Arctic and Antarctic Adminis- tration for fieldwork support. Article in Journal/Newspaper Antarc* Antarctic Arctic Arctic Ocean Sea ice Digital.CSIC (Spanish National Research Council) Antarctic Arctic Arctic Ocean Science of The Total Environment 834 155030 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
unknown |
topic |
Arctic Ocean Iodine chemistry Single particle Sea ice Diurnal trends |
spellingShingle |
Arctic Ocean Iodine chemistry Single particle Sea ice Diurnal trends Wang, Longquan Yan, Jingpei Saiz-Lopez, A. Jiang, Bei Yue, Fange Yu, Xiawei Xie, Zhouqing Mixing state and distribution of iodine-containing particles in Arctic Ocean during summertime |
topic_facet |
Arctic Ocean Iodine chemistry Single particle Sea ice Diurnal trends |
description |
10 pags., 6 figs., 1 tab. Iodine chemistry plays a key role in ozone destruction and new aerosol formation in the marine boundary layer (MBL), especially in polar regions. We investigated iodine-containing particles (0.2-2 μm) in the Arctic Ocean using a ship-based single particle aerosol mass spectrometer from July to August 2017. Seven main particle types were identified: dust, biomass combustion particles, sea salt, organic S, aromatics, hydrocarbon-like compounds, and amines. The number fraction of iodine-containing particles was higher inside the Arctic Circle (>65°N) than outside (55–65°N). According to the air mass back trajectories, the latitudinal distribution of iodine-containing particles can be mainly attributed to iodine emissions from the sea ice edge region. Diurnal trends were found, especially during the second half of cruise, with peak iodine-containing particle number fractions during low-light conditions and relatively low number fractions at midday. These results imply that solar radiation plays a significant role in modulating particulate iodine in the Arctic atmosphere. This work was supported by the National Natural Science Foundation of China (NSFC) (41941014). We thank China Arctic and Antarctic Adminis- tration for fieldwork support. |
author2 |
National Natural Science Foundation of China |
format |
Article in Journal/Newspaper |
author |
Wang, Longquan Yan, Jingpei Saiz-Lopez, A. Jiang, Bei Yue, Fange Yu, Xiawei Xie, Zhouqing |
author_facet |
Wang, Longquan Yan, Jingpei Saiz-Lopez, A. Jiang, Bei Yue, Fange Yu, Xiawei Xie, Zhouqing |
author_sort |
Wang, Longquan |
title |
Mixing state and distribution of iodine-containing particles in Arctic Ocean during summertime |
title_short |
Mixing state and distribution of iodine-containing particles in Arctic Ocean during summertime |
title_full |
Mixing state and distribution of iodine-containing particles in Arctic Ocean during summertime |
title_fullStr |
Mixing state and distribution of iodine-containing particles in Arctic Ocean during summertime |
title_full_unstemmed |
Mixing state and distribution of iodine-containing particles in Arctic Ocean during summertime |
title_sort |
mixing state and distribution of iodine-containing particles in arctic ocean during summertime |
publisher |
Elsevier |
publishDate |
2022 |
url |
http://hdl.handle.net/10261/280314 https://doi.org/10.1016/j.scitotenv.2022.155030 https://doi.org/10.13039/501100001809 |
geographic |
Antarctic Arctic Arctic Ocean |
geographic_facet |
Antarctic Arctic Arctic Ocean |
genre |
Antarc* Antarctic Arctic Arctic Ocean Sea ice |
genre_facet |
Antarc* Antarctic Arctic Arctic Ocean Sea ice |
op_relation |
Postprint http://dx.doi.org/10.1016/j.scitotenv.2022.155030 Sí doi:10.1016/j.scitotenv.2022.155030 issn: 1879-1026 Science of the Total Environment 834: 155030 (2022) http://hdl.handle.net/10261/280314 http://dx.doi.org/10.13039/501100001809 |
op_rights |
embargo_20240404 |
op_doi |
https://doi.org/10.1016/j.scitotenv.2022.15503010.13039/501100001809 |
container_title |
Science of The Total Environment |
container_volume |
834 |
container_start_page |
155030 |
_version_ |
1790608521597812736 |