Articles | Volume 26, issue 19
https://doi.org/10.5194/acp-26-13983-2026
https://doi.org/10.5194/acp-26-13983-2026
Research article
 | 
06 Oct 2026
Research article |  | 06 Oct 2026

Impacts of mesoscale atmospheric subsidence on cloud glaciation and decoupling in Arctic marine cold air outbreaks

Fiona Paulus, Joshua J. Müller, Benjamin Kirbus, Harald Sodemann, Lars van Gelder, Andreas Walbröl, Manfred Wendisch, and Roel A. J. Neggers

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Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Fiona Paulus on behalf of the Authors (28 Jul 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (29 Jul 2026) by Ivy Tan
RR by Anonymous Referee #1 (07 Aug 2026)
RR by Anonymous Referee #2 (17 Aug 2026)
ED: Publish subject to technical corrections (17 Aug 2026) by Ivy Tan
AR by Fiona Paulus on behalf of the Authors (21 Aug 2026)  Author's response   Manuscript 
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Short summary
Cold Arctic air flowing from sea ice onto the warmer ocean waters rapidly warms, moistens, and forms clouds and precipitation. These events shape the Arctic climate but are difficult to observe and model. Particularly the role of large-scale sinking motion during these events is not fully understood. Using rare aircraft data and simulations to track an air mass for two days, we show that strong downward motion suppresses cloud growth, limits and delays precipitation, and reduces cloud lifetimes.
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