Articles | Volume 25, issue 12
Hydrol. Earth Syst. Sci., 25, 6309–6332, 2021
https://doi.org/10.5194/hess-25-6309-2021

Special issue: Assessing impacts and adaptation to global change in water...

Hydrol. Earth Syst. Sci., 25, 6309–6332, 2021
https://doi.org/10.5194/hess-25-6309-2021

Research article 13 Dec 2021

Research article | 13 Dec 2021

Use of water isotopes and chemistry to infer the type and degree of exchange between groundwater and lakes in an esker complex of northeastern Ontario, Canada

Maxime P. Boreux et al.

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (18 Dec 2017) by Nandita Basu
AR by Maxime Boreux on behalf of the Authors (27 Mar 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (08 Apr 2018) by Nandita Basu
RR by Anonymous Referee #3 (21 May 2018)
RR by Kevin Turner (05 Jun 2018)
ED: Reconsider after major revisions (further review by editor and referees) (19 Jul 2018) by Nandita Basu
AR by Anna Wenzel on behalf of the Authors (09 Jan 2019)  Author's response    Manuscript
ED: Publish subject to revisions (further review by editor and referees) (02 Feb 2019) by Nandita Basu
AR by Svenja Lange on behalf of the Authors (25 Mar 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (15 Apr 2019) by Nandita Basu
RR by Anonymous Referee #3 (20 May 2019)
ED: Publish subject to minor revisions (review by editor) (29 Jun 2019) by Nandita Basu
AR by Maxime Boreux on behalf of the Authors (12 Jul 2019)  Author's response
ED: Publish as is (09 Aug 2019) by Nandita Basu

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Maxime Boreux on behalf of the Authors (20 May 2021)   Author's adjustment   Manuscript
EA: Adjustments approved (03 Jul 2021) by Alberto Guadagnini
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Short summary
The investigation of groundwater–lake-water interactions in highly permeable boreal terrain using several indicators showed that lowland lakes are embedded into the groundwater system and are thus relatively resilient to short-term hydroclimatic change, while upland lakes rely more on precipitation as their main water input, making them more sensitive to evaporative drawdown. This suggests that landscape position controls the vulnerability of lake-water levels to hydroclimatic change.