Articles | Volume 29, issue 17
https://doi.org/10.5194/hess-29-4241-2025
https://doi.org/10.5194/hess-29-4241-2025
Research article
 | 
09 Sep 2025
Research article |  | 09 Sep 2025

Rainfall recharge thresholds decrease after an intense fire over a near-surface cave at Wombeyan, Australia

Christina Song, Micheline Campbell, and Andy Baker

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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-2025-84', Anonymous Referee #1, 21 Mar 2025
    • AC2: 'Reply on RC1', Andy Baker, 22 Apr 2025
  • RC2: 'Comment on egusphere-2025-84', Anonymous Referee #2, 14 Apr 2025
    • AC1: 'Reply on RC2', Andy Baker, 22 Apr 2025
  • CC1: 'Comment on egusphere-2025-84', Bryce Belanger, 23 Apr 2025
    • AC3: 'Reply on CC1', Andy Baker, 05 May 2025
  • RC3: 'Comment on egusphere-2025-84', Anonymous Referee #3, 23 May 2025
    • AC4: 'Reply on RC3', Andy Baker, 13 Jun 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (further review by editor) (13 Jun 2025) by Gerrit H. de Rooij
AR by Andy Baker on behalf of the Authors (22 Jun 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (24 Jun 2025) by Gerrit H. de Rooij
AR by Andy Baker on behalf of the Authors (26 Jun 2025)
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Short summary
Groundwater can be replenished by rainfall that percolates from the surface to the water table. The amount of rainfall that is needed to generate this groundwater recharge is hard to measure. We determined this rainfall amount by identifying recharge events as water percolates from the surface, through a cave. During our monitoring, an intense fire occurred above the cave, and we were able to quantify any change in the amount of rainfall necessary to generate recharge before and after the fire.
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