Articles | Volume 19, issue 15
https://doi.org/10.5194/gmd-19-7197-2026
https://doi.org/10.5194/gmd-19-7197-2026
Development and technical paper
 | 
05 Aug 2026
Development and technical paper |  | 05 Aug 2026

DReaMIT: a dynamical reanalysis framework for modelling surface-based temperature inversions in cold environments

Victor Pozsgay, Nick Noad, Philip Bonnaventure, and Stephan Gruber

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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-2025-5512', Anonymous Referee #1, 28 May 2026
    • AC1: 'Reply on RC1', Victor Pozsgay, 11 Jun 2026
  • RC2: 'Comment on egusphere-2025-5512', Anonymous Referee #2, 02 Jun 2026
    • AC2: 'Reply on RC2', Victor Pozsgay, 11 Jun 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Victor Pozsgay on behalf of the Authors (12 Jun 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (12 Jun 2026) by Chiel van Heerwaarden
RR by Anonymous Referee #1 (27 Jul 2026)
ED: Publish as is (28 Jul 2026) by Chiel van Heerwaarden
AR by Victor Pozsgay on behalf of the Authors (30 Jul 2026)  Manuscript 
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Short summary
Surface-based temperature inversions occur when cold air becomes trapped near the ground beneath a layer of warmer air. This study combines field data, analysis, and modelling to develop DReaMIT, a model that captures the timing and strength of inversions across northern mountain terrain. The model's transferability beyond the valleys where it was developed makes it valuable globally to cold-region researchers for mapping and modelling permafrost and assessing climate change impacts.
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