Preprints
https://doi.org/10.5194/egusphere-2025-4866
https://doi.org/10.5194/egusphere-2025-4866
21 Oct 2025
 | 21 Oct 2025
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Measurement report: Role of Organic Coating and Chemical Composition on Ice Nucleation Potential of Atmospheric Particles in European Arctic

Nurun Nahar Lata, Trung Diep, Stefania Gilardoni, Mauro Mazzola, Zezhen Cheng, Ashfiqur Rahman, Mickey Rogers, Matthew Fraund, Matthew Marcus, Naruki Hiranuma, and Swarup China

Abstract. Understanding the ice nucleation (IN) potential of Arctic aerosols is critical for predicting their influence on cloud formation and water cycles in this vulnerable region. This study investigates the role of particle composition, organic coatings, and aerosol sources in modulating IN activity across five aerosol samples collected at the Gruvebadet Observatory Station in Ny-Ålesund, Svalbard. The IN potential of Arctic aerosol particles was studied by investigating chemical, morphological, and ice activity measurements. Single-particle analyses revealed distinct differences in mixing state, organic volume fraction (OVF), and organic coating morphology across samples. OVF distributions were linked to particle origin, with marine-influenced Na-rich particles often exhibiting thin organic coatings, while long-range transported particles showed thicker organic coatings. Biogenic contributions, though variable, were linked to heat-sensitive INPs, suggesting a role for labile biological macromolecules under certain meteorological conditions. Pearson correlation analysis between particle composition and immersion-mode ice-nucleating particle (INP) concentrations at two freezing temperatures indicated that organic-rich and Na-rich particles were positively associated with enhanced ice activity. However, discrepancies in INP activity were observed for particles with thicker organic coatings, where the morphological configuration of the organic material may play a role. The results highlight that Arctic INP variability is governed not only by chemical composition but also by the morphological configuration of organic material, which can either enhance or inhibit ice nucleation depending on its abundance, distribution, thickness, and mixing state. These findings underscore the combined influence of source regions, atmospheric processing, and organic–inorganic interactions in shaping Arctic aerosol freezing behavior.

Competing interests: Some authors are members of the editorial board of journal ACP.

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Nurun Nahar Lata, Trung Diep, Stefania Gilardoni, Mauro Mazzola, Zezhen Cheng, Ashfiqur Rahman, Mickey Rogers, Matthew Fraund, Matthew Marcus, Naruki Hiranuma, and Swarup China

Status: open (until 02 Dec 2025)

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Nurun Nahar Lata, Trung Diep, Stefania Gilardoni, Mauro Mazzola, Zezhen Cheng, Ashfiqur Rahman, Mickey Rogers, Matthew Fraund, Matthew Marcus, Naruki Hiranuma, and Swarup China

Data sets

Data set for Measurement report: Role of Organic Coating and Chemical Composition on Ice Nucleation Potential of Atmospheric Particles in European Arctic N. N. Lata et al. https://doi.org/10.5281/zenodo.17373230

Nurun Nahar Lata, Trung Diep, Stefania Gilardoni, Mauro Mazzola, Zezhen Cheng, Ashfiqur Rahman, Mickey Rogers, Matthew Fraund, Matthew Marcus, Naruki Hiranuma, and Swarup China
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Latest update: 21 Oct 2025
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Short summary
Ice in the Arctic clouds is initiated by rare particles, and their properties are not well understood due to atmospheric processing. By combining microscopy with freezing experiments, we found that both chemical composition and the thickness and morphological configuration of organic coatings influence ice formation. This finding highlights the importance of particle surface chemistry in cloud formation and offers new insights into how Arctic aerosols influence cloud formation.
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