Articles | Volume 4, issue 1
https://doi.org/10.5194/wcd-4-157-2023
https://doi.org/10.5194/wcd-4-157-2023
Research article
 | 
25 Jan 2023
Research article |  | 25 Jan 2023

Origin of low-tropospheric potential vorticity in Mediterranean cyclones

Alexander Scherrmann, Heini Wernli, and Emmanouil Flaounas

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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 wcd-2022-40', Anonymous Referee #1, 23 Jul 2022
  • RC2: 'Comment on wcd-2022-40', Anonymous Referee #2, 22 Aug 2022
  • AC1: 'Reply to the Reviewers' comments on wcd-2022-40', Alexander Scherrmann, 29 Sep 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Alexander Scherrmann on behalf of the Authors (24 Nov 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (09 Dec 2022) by Juliane Schwendike
RR by Anonymous Referee #1 (20 Dec 2022)
ED: Publish as is (09 Jan 2023) by Juliane Schwendike
AR by Alexander Scherrmann on behalf of the Authors (10 Jan 2023)  Manuscript 
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Short summary
We investigate the dynamical origin of the lower-atmospheric potential vorticity (PV; linked to the intensity of cyclones) in Mediterranean cyclones. We quantify the contribution of the cyclone and the environment by tracing PV backward in time and space and linking it to the track of the cyclone. We find that the lower-tropospheric PV is produced shortly before the cyclone's stage of highest intensity. We investigate the driving processes and use a global dataset and a process-resolving one.