Articles | Volume 26, issue 13
https://doi.org/10.5194/acp-26-9625-2026
https://doi.org/10.5194/acp-26-9625-2026
Research article
 | 
08 Jul 2026
Research article |  | 08 Jul 2026

Mesoscale modulation of marine boundary layer water vapor isotopologues during EUREC4A

Joseph Galewsky and Sebastian A. Los

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Joe Galewsky on behalf of the Authors (09 Jan 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (15 Jan 2026) by Kara Lamb
RR by Anonymous Referee #2 (06 Feb 2026)
RR by Anonymous Referee #1 (23 Mar 2026)
ED: Reconsider after major revisions (31 Mar 2026) by Kara Lamb
AR by Joe Galewsky on behalf of the Authors (11 May 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (01 Jun 2026) by Kara Lamb
RR by Anonymous Referee #2 (13 Jun 2026)
ED: Publish subject to technical corrections (16 Jun 2026) by Kara Lamb
AR by Joe Galewsky on behalf of the Authors (22 Jun 2026)  Manuscript 
Download
Short summary
This study shows that organized air motions over the tropical ocean can strongly shape the character of near-surface water vapor, even when overall moisture changes little. By combining ship and aircraft measurements with a simple physical model, we found that rising air can offset drying from mixing with air above, leaving a clear chemical fingerprint. These results help explain why clouds persist and improve how climate models represent them.
Share
Altmetrics
Final-revised paper
Preprint