Articles | Volume 26, issue 5
https://doi.org/10.5194/hess-26-1459-2022
https://doi.org/10.5194/hess-26-1459-2022
Research article
 | 
16 Mar 2022
Research article |  | 16 Mar 2022

Combining passive and active distributed temperature sensing measurements to locate and quantify groundwater discharge variability into a headwater stream

Nataline Simon, Olivier Bour, Mikaël Faucheux, Nicolas Lavenant, Hugo Le Lay, Ophélie Fovet, Zahra Thomas, and Laurent Longuevergne

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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-2021-293', B. des Tombe, 15 Jul 2021
    • AC1: 'Reply on RC1', Nataline Simon, 28 Oct 2021
  • RC2: 'Comment on hess-2021-293', Stefan Ploum, 28 Sep 2021
    • AC2: 'Reply on RC2', Nataline Simon, 28 Oct 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (01 Nov 2021) by Miriam Coenders-Gerrits
AR by Nataline Simon on behalf of the Authors (21 Dec 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (23 Dec 2021) by Miriam Coenders-Gerrits
RR by B.F. des Tombe (22 Jan 2022)
ED: Publish subject to minor revisions (review by editor) (04 Feb 2022) by Miriam Coenders-Gerrits
AR by Nataline Simon on behalf of the Authors (10 Feb 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (14 Feb 2022) by Miriam Coenders-Gerrits
AR by Nataline Simon on behalf of the Authors (18 Feb 2022)
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Short summary
Groundwater discharge into streams plays a major role in the preservation of stream ecosystems. There were two complementary methods, both based on the use of the distributed temperature sensing technology, applied in a headwater catchment. Measurements allowed us to characterize the spatial and temporal patterns of groundwater discharge and quantify groundwater inflows into the stream, opening very promising perspectives for a novel characterization of the groundwater–stream interface.