Articles | Volume 26, issue 3
https://doi.org/10.5194/acp-26-2331-2026
https://doi.org/10.5194/acp-26-2331-2026
Research article
 | 
16 Feb 2026
Research article |  | 16 Feb 2026

Microphysics of Arctic Stratiform Boundary-layer Clouds during ARCSIX

Alexei V. Korolev and R. Paul Lawson

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Short summary
The International Panel on Climate Change has concluded that aerosols and clouds are significant contributors to the rate of warming in the Arctic, which is now shown to be more than twice that of the global average. Climate model predictions suggest that the Arctic Ocean will become ice-free sometime between 2030 and 2050. The research presented here increases our knowledge of how aerosols, clouds and surface properties contribute to warming and the melting of sea ice in the Arctic.
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