Articles | Volume 26, issue 13
https://doi.org/10.5194/acp-26-9657-2026
https://doi.org/10.5194/acp-26-9657-2026
Research article
 | 
09 Jul 2026
Research article |  | 09 Jul 2026

Aircraft-derived particle fluxes distinguish entrainment zone and decoupled layer nucleation in marine boundary layers

Ajmal Rasheeda Satheesh, Markus D. Petters, and Nicholas Meskhidze

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2026-61', Anonymous Referee #1, 04 Mar 2026
  • RC2: 'Comment on egusphere-2026-61', Anonymous Referee #2, 20 Mar 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Nicholas Meskhidze on behalf of the Authors (18 May 2026)  Author's response   Author's tracked changes   Manuscript 
EF by Mario Ebel (18 May 2026)  Supplement 
ED: Referee Nomination & Report Request started (18 May 2026) by Radovan Krejci
RR by Anonymous Referee #2 (09 Jun 2026)
ED: Publish subject to minor revisions (review by editor) (10 Jun 2026) by Radovan Krejci
AR by Nicholas Meskhidze on behalf of the Authors (12 Jun 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (15 Jun 2026) by Radovan Krejci
AR by Nicholas Meskhidze on behalf of the Authors (22 Jun 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (23 Jun 2026) by Radovan Krejci
AR by Nicholas Meskhidze on behalf of the Authors (26 Jun 2026)
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Short summary
Using aircraft data collected over the Atlantic Ocean, we discovered that new particles form regularly in marine air at two different heights, challenging the belief that sea salt prevents this process. These particles can grow to form cloud droplets, affecting Earth's climate. We found particles forming at two heights: where upper atmosphere air enters the ocean boundary layer and where the well-mixed surface air meets the stable air layer above. This discovery will help improve climate models.
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