Articles | Volume 24, issue 8
https://doi.org/10.5194/acp-24-5009-2024
https://doi.org/10.5194/acp-24-5009-2024
Research article
 | 
29 Apr 2024
Research article |  | 29 Apr 2024

Distribution and morphology of non-persistent contrail and persistent contrail formation areas in ERA5

Kevin Wolf, Nicolas Bellouin, and Olivier Boucher

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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-2023-3086', Anonymous Referee #1, 27 Jan 2024
    • AC1: 'Reply on RC1', Kevin Wolf, 04 Mar 2024
  • RC2: 'Comment on egusphere-2023-3086', Anonymous Referee #2, 14 Feb 2024
    • AC2: 'Reply on RC2', Kevin Wolf, 04 Mar 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Kevin Wolf on behalf of the Authors (04 Mar 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (18 Mar 2024) by Michael Tjernström
AR by Kevin Wolf on behalf of the Authors (18 Mar 2024)  Author's response   Manuscript 
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Short summary
The contrail formation potential and its tempo-spatial distribution are estimated for the North Atlantic flight corridor. Meteorological conditions of temperature and relative humidity are taken from the ERA5 re-analysis and IAGOS. Based on IAGOS flight tracks, crossing length, size, orientation, frequency of occurrence, and overlap of persistent contrail formation areas are determined. The presented conclusions might provide a guide for statistical flight track optimization to reduce contrails.
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