Articles | Volume 24, issue 13
https://doi.org/10.5194/acp-24-7731-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-24-7731-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Jul 2024
Research article |
| 09 Jul 2024
| 09 Jul 2024
Diverse sources and aging change the mixing state and ice nucleation properties of aerosol particles over the western Pacific and Southern Ocean
State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen, 361102, China
Tian Zhang
State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen, 361102, China
Keyhong Park
Korea Polar Research Institute, Incheon, 21990, South Korea
Jinpei Yan
Third Institute of Oceanography, Ministry of Natural Resources, Xiamen 361005, China
Young Jun Yoon
Korea Polar Research Institute, Incheon, 21990, South Korea
Jiyeon Park
CORRESPONDING AUTHOR
Korea Polar Research Institute, Incheon, 21990, South Korea
Bingbing Wang
CORRESPONDING AUTHOR
State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen, 361102, China
Center for Marine Meteorology and Climate Change, Xiamen University, Xiamen, 361102, China
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Short summary
Ice formation by particles is an important way of making mixed-phase and ice clouds. We found that particles collected in the marine atmosphere exhibit diverse ice nucleation abilities and mixing states. Sea salt mixed-sulfate particles were enriched in ice-nucleating particles. Selective aging on sea salt particles made particle populations more externally mixed. Characterizations of particles and their mixing state are needed for a better understanding of aerosol–cloud interactions.
Ice formation by particles is an important way of making mixed-phase and ice clouds. We found...
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