Articles | Volume 25, issue 12
Hydrol. Earth Syst. Sci., 25, 6261–6281, 2021
https://doi.org/10.5194/hess-25-6261-2021
Hydrol. Earth Syst. Sci., 25, 6261–6281, 2021
https://doi.org/10.5194/hess-25-6261-2021

Research article 13 Dec 2021

Research article | 13 Dec 2021

Identification of the contributing area to river discharge during low-flow periods

Maxime Gillet et al.

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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-2021-267', Anonymous Referee #1, 28 Jun 2021
    • AC1: 'Reply on RC1', Maxime Gillet, 07 Sep 2021
  • RC2: 'Comment on hess-2021-267', Anonymous Referee #2, 29 Jul 2021
    • AC2: 'Reply on RC2', Maxime Gillet, 07 Sep 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (14 Sep 2021) by Markus Hrachowitz
AR by Maxime Gillet on behalf of the Authors (12 Oct 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (12 Oct 2021) by Markus Hrachowitz
RR by Anonymous Referee #1 (05 Nov 2021)
ED: Publish as is (09 Nov 2021) by Markus Hrachowitz
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Short summary
This paper aims at identifying the key reservoirs sustaining river low flow during dry summer. The reservoirs are discriminated based on the geological nature of the formations and the geochemical signature of groundwater. Results show the increasing importance to low-flow support of a specific reservoir, showing only a limited outcrop area and becoming preponderant in the heart of the dry season. This finding will contribute to improving the protective measures for preserving low flows.