Measurement report: Atmospheric ice nuclei in the Changbai Mountains (2623&thinsp;m&thinsp;a.s.l.) in northeastern Asia

Sun, Yue; Zhu, Yujiao; Qi, Yanbin; Chen, Lanxiadi; Mu, Jiangshan; Shan, Ye; Yang, Yu; Nie, Yanqiu; Liu, Ping; Cui, Can; Zhang, Ji; Liu, Mingxuan; Zhang, Lingli; Wang, Yufei; Wang, Xinfeng; Tang, Mingjin; Wang, Wenxing; Xue, Likun

doi:https://doi.org/10.5194/acp-24-3241-2024

Articles | Volume 24, issue 5

https://doi.org/10.5194/acp-24-3241-2024

© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/acp-24-3241-2024

© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 24, issue 5

Measurement report

|

15 Mar 2024

Measurement report |

| 15 Mar 2024

Measurement report: Atmospheric ice nuclei in the Changbai Mountains (2623 m a.s.l.) in northeastern Asia

Yue Sun, Yujiao Zhu, Yanbin Qi, Lanxiadi Chen, Jiangshan Mu, Ye Shan, Yu Yang, Yanqiu Nie, Ping Liu, Can Cui, Ji Zhang, Mingxuan Liu, Lingli Zhang, Yufei Wang, Xinfeng Wang, Mingjin Tang, Wenxing Wang, and Likun Xue

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Oct 2024	58	12	4	74
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Cumulative views and downloads (calculated since 15 Jun 2023)

Month	HTML	PDF	XML	Total
Jun 2023	106	42	4	152
Jul 2023	73	25	3	101
Aug 2023	44	15	4	63
Sep 2023	43	17	2	62
Oct 2023	53	27	8	88
Nov 2023	24	12	1	37
Dec 2023	47	31	5	83
Jan 2024	44	20	1	65
Feb 2024	11	16	1	28
Mar 2024	283	69	12	364
Apr 2024	73	19	6	98
May 2024	54	17	2	73
Jun 2024	85	11	4	100
Jul 2024	59	24	4	87
Aug 2024	32	9	2	43
Sep 2024	40	8	0	48
Oct 2024	58	12	4	74
Nov 2024	59	8	1	68
Dec 2024	50	15	1	66
Jan 2025	42	15	1	58
Feb 2025	40	8	2	50
Mar 2025	27	5	0	32
Apr 2025	35	9	1	45
May 2025	74	10	0	84
Jun 2025	80	9	0	89
Jul 2025	32	17	2	51

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Short summary

Field observations were conducted at the summit of Changbai Mountain in northeast Asia. The cumulative number concentration of ice-nucleating particles (INPs) varied from 1.6 × 10⁻³ to 78.3 L⁻¹ over the temperature range of −5.5 to −29.0 ℃. Biological INPs (bio-INPs) accounted for the majority of INPs, and the proportion exceeded 90% above −13.0 ℃. Planetary boundary layer height, valley breezes, and long-distance transport of air mass influence the abundance of bio-INPs.