Contrasting aerosol–cloud feedbacks across a warming Arctic

Abstract In the rapidly warming Arctic, the feedback between aerosols and clouds is a major source of uncertainty in projections of future climate. One source of this uncertainty is the role of new particle formation, which produces aerosol particles that can subsequently grow into cloud condensation nuclei, thereby influencing Arctic cloud formation. Here harmonized field aerosol observations across the Arctic spanning 2003–2024, alongside satellite-derived data, were analysed to quantify trends in new particle formation and estimate their climatic implications across the Arctic region. Three distinct aerosol regimes, with contrasting contributions of new particle formation to cloud condensation nuclei populations, were identified: the High Arctic, the Maritime Arctic and the Continental Arctic. In these three regimes, temperature-sensitivity estimates based on the intermediate future warming scenario suggest that by 2090–2100, cloud condensation nuclei concentrations associated with new particle formation activity could increase by 3–16% in the High Arctic but decline by 15–31% in the Maritime Arctic. These contrasting estimates indicate that aerosol–cloud feedbacks will evolve differently across the mosaic of Arctic aerosol regimes.

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Publication Details

Journal
Nature Geoscience
Published
2026-09-28
DOI
https://doi.org/10.1038/s41561-026-02114-x
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
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article

Contrasting aerosol–cloud feedbacks across a warming Arctic

Lynn Monica Russell, Katrianne Lehtipalo, Radovan Krejčí, Peter Tunved et al.
Nature Geoscience
Atmospheric aerosols and clouds
article

Contrasting aerosol–cloud feedbacks across a warming Arctic

Lynn Monica Russell, Katrianne Lehtipalo, Radovan Krejčí, Peter Tunved, Antti Hyvärinen, Herbert Hartl, Henrik Skov, Mikko Sipilä, Nina Sarnela, Samuel De Xun Chua, Sourita Saha, Eija Asmi, Ville Vakkari, Andreas Maßling, Tuukka Petäjä, Veli‐Matti Kerminen, Martha Arbayani Zaidan, Christina J. Williamson, Paul Zieger, Tak Chan, John Backman, Julia Kojoj, Ilona Jaakkola, Jakob Boyd Pernov, Matthew Boyer
article en

Abstract

Abstract In the rapidly warming Arctic, the feedback between aerosols and clouds is a major source of uncertainty in projections of future climate. One source of this uncertainty is the role of new particle formation, which produces aerosol particles that can subsequently grow into cloud condensation nuclei, thereby influencing Arctic cloud formation. Here harmonized field aerosol observations across the Arctic spanning 2003–2024, alongside satellite-derived data, were analysed to quantify trends in new particle formation and estimate their climatic implications across the Arctic region. Three distinct aerosol regimes, with contrasting contributions of new particle formation to cloud condensation nuclei populations, were identified: the High Arctic, the Maritime Arctic and the Continental Arctic. In these three regimes, temperature-sensitivity estimates based on the intermediate future warming scenario suggest that by 2090–2100, cloud condensation nuclei concentrations associated with new particle formation activity could increase by 3–16% in the High Arctic but decline by 15–31% in the Maritime Arctic. These contrasting estimates indicate that aerosol–cloud feedbacks will evolve differently across the mosaic of Arctic aerosol regimes.

Nature Geoscience
Finnish Meteorological Institute (FI), University of Helsinki (FI), Environment and Climate Change Canada (CA), Scripps Institution of Oceanography (US), Queensland University of Technology (AU), Stockholm University (SE), Aarhus University (DK), North-West University (ZA), University of California San Diego (US), Bolin Centre for Climate Research (SE), École Polytechnique Fédérale de Lausanne (CH)
Climate action
Openalex Percentile: Top 15%
Atmospheric aerosols and clouds
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