Articles | Volume 5, issue 4
https://doi.org/10.5194/wcd-5-1457-2024
https://doi.org/10.5194/wcd-5-1457-2024
Research article
 | 
12 Nov 2024
Research article |  | 12 Nov 2024

Dynamic and thermodynamic contribution to the October 2019 exceptional rainfall in western central Africa

Kevin Kenfack, Francesco Marra, Zéphirin Yepdo Djomou, Lucie Angennes Djiotang Tchotchou, Alain Tchio Tamoffo, and Derbetini Appolinaire Vondou

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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-2024-1257', Anonymous Referee #1, 03 Jun 2024
    • AC1: 'Reply on RC1', Kevin Kenfack, 13 Jul 2024
  • RC2: 'Comment on egusphere-2024-1257', Anonymous Referee #2, 20 Jun 2024
    • AC2: 'Reply on RC2', Kevin Kenfack, 13 Jul 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Kevin Kenfack on behalf of the Authors (17 Jul 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (30 Jul 2024) by Martin Singh
RR by Anonymous Referee #1 (19 Aug 2024)
RR by Anonymous Referee #2 (19 Aug 2024)
ED: Publish subject to minor revisions (review by editor) (21 Aug 2024) by Martin Singh
AR by Kevin Kenfack on behalf of the Authors (27 Aug 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (13 Sep 2024) by Martin Singh
AR by Kevin Kenfack on behalf of the Authors (14 Sep 2024)  Manuscript 
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Short summary
The results of this study show that moisture advection induced by horizontal wind anomalies and vertical moisture advection induced by vertical velocity anomalies were crucial mechanisms behind the anomalous October 2019 exceptional rainfall increase over western central Africa. The information we derive can be used to support risk assessment and management in the region and to improve our resilience to ongoing climate change.