Articles | Volume 26, issue 12
https://doi.org/10.5194/acp-26-8455-2026
https://doi.org/10.5194/acp-26-8455-2026
Research article
 | 
17 Jun 2026
Research article |  | 17 Jun 2026

Boundary layer dynamics after rain fronts: high-resolution reconstruction and model validation using ground- and drone-based measurements

Lasse Moormann, Friederike Fachinger, Frank Drewnick, and Holger Tost

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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-2025-3862', Anonymous Referee #1, 14 Nov 2025
  • RC2: 'Comment on egusphere-2025-3862', Anonymous Referee #2, 18 Nov 2025

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Lasse Moormann on behalf of the Authors (19 Jan 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (23 Feb 2026) by Annika Oertel
RR by Anonymous Referee #2 (10 Mar 2026)
RR by Anonymous Referee #1 (20 Mar 2026)
ED: Reconsider after major revisions (30 Mar 2026) by Annika Oertel
AR by Lasse Moormann on behalf of the Authors (27 Apr 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (22 May 2026) by Annika Oertel
RR by Anonymous Referee #2 (28 May 2026)
ED: Publish subject to minor revisions (review by editor) (29 May 2026) by Annika Oertel
AR by Lasse Moormann on behalf of the Authors (02 Jun 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (02 Jun 2026) by Annika Oertel
AR by Lasse Moormann on behalf of the Authors (03 Jun 2026)  Manuscript 

Post-review adjustments

AA – Author's adjustment | EA – Editor approval
AA by Lasse Moormann on behalf of the Authors (16 Jun 2026)   Author's adjustment   Manuscript
EA: Adjustments approved (16 Jun 2026) by Annika Oertel
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Short summary
We examine boundary layer (BL) processes during summer rain in Germany, focusing on air mass exchange and precipitation effects. Using drone and ground observations, and ICON (ICOsahedral Nonhydrostatic) model data, we link delayed BL breakup and weak vertical mixing to aerosol formation and chemical processes. ICON predicts mixing layer height under stable conditions but underestimates it during cold pool events, enhancing understanding of frontal weather scenarios and atmospheric changes.
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