Articles | Volume 26, issue 1
https://doi.org/10.5194/hess-26-183-2022
https://doi.org/10.5194/hess-26-183-2022
Research article
 | 
14 Jan 2022
Research article |  | 14 Jan 2022

Implications of variations in stream specific conductivity for estimating baseflow using chemical mass balance and calibrated hydrograph techniques

Ian Cartwright

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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-2021-454', Anonymous Referee #1, 02 Nov 2021
    • AC1: 'Reply to Reviewer 1', Ian Cartwright, 22 Nov 2021
  • RC2: 'Review 2', Anonymous Referee #2, 04 Nov 2021
    • AC2: 'Response to Reviewer 2', Ian Cartwright, 22 Nov 2021

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) (22 Nov 2021) by Genevieve Ali
AR by Ian Cartwright on behalf of the Authors (29 Nov 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (10 Dec 2021) by Genevieve Ali
AR by Ian Cartwright on behalf of the Authors (13 Dec 2021)
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Short summary
Using specific conductivity (SC) to estimate groundwater inflow to rivers is complicated by bank return waters, interflow, and flows off floodplains contributing to baseflow in all but the driest years. Using the maximum SC of the river in dry years to estimate the SC of groundwater produces the best baseflow vs. streamflow trends. The variable composition of baseflow hinders calibration of hydrograph-based techniques to estimate groundwater inflows.