Articles | Volume 26, issue 16
https://doi.org/10.5194/hess-26-4391-2022
https://doi.org/10.5194/hess-26-4391-2022
Research article
 | 
26 Aug 2022
Research article |  | 26 Aug 2022

Recession discharge from compartmentalized bedrock hillslopes

Clément Roques, David E. Rupp, Jean-Raynald de Dreuzy, Laurent Longuevergne, Elizabeth R. Jachens, Gordon Grant, Luc Aquilina, and John S. Selker

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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 hess-2022-7', Anonymous Referee #1, 29 Mar 2022
    • AC1: 'Reply on RC1', Clement Roques, 13 Jun 2022
  • RC2: 'Comment on hess-2022-7', Anonymous Referee #2, 20 May 2022
    • AC2: 'Reply on RC2', Clement Roques, 13 Jun 2022

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) (24 Jul 2022) by Patricia Saco
AR by Clement Roques on behalf of the Authors (03 Aug 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (04 Aug 2022) by Patricia Saco
AR by Clement Roques on behalf of the Authors (16 Aug 2022)
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Short summary
Streamflow dynamics are directly dependent on contributions from groundwater, with hillslope heterogeneity being a major driver in controlling both spatial and temporal variabilities in recession discharge behaviors. By analysing new model results, this paper identifies the major structural features of aquifers driving streamflow dynamics. It provides important guidance to inform catchment-to-regional-scale models, with key geological knowledge influencing groundwater–surface water interactions.