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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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HESS | Articles | Volume 22, issue 12
Hydrol. Earth Syst. Sci., 22, 6163–6185, 2018
https://doi.org/10.5194/hess-22-6163-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Hydrol. Earth Syst. Sci., 22, 6163–6185, 2018
https://doi.org/10.5194/hess-22-6163-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Review article 30 Nov 2018

Review article | 30 Nov 2018

Toward a conceptual framework of hyporheic exchange across spatial scales

Chiara Magliozzi et al.

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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: Publish subject to minor revisions (further review by editor) (11 Oct 2018) by Thom Bogaard
AR by Chiara Magliozzi on behalf of the Authors (19 Oct 2018)  Author's response    Manuscript
ED: Publish as is (28 Oct 2018) by Thom Bogaard
Publications Copernicus
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Short summary
The hyporheic zone is the area below riverbeds where surfacewater and groundwater mix. Hyporheic flow is linked to river processes and functions, but research to date has not sufficiently addressed how factors operating at different scales in time and space drive hyporheic flow variations at reach and larger scales. This review presents the scale-specific processes and interactions that control hyporheic flow, and a case study showing how valley factors affect its expression at the reach scale.
The hyporheic zone is the area below riverbeds where surfacewater and groundwater mix. Hyporheic...
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