Articles | Volume 22, issue 12
https://doi.org/10.5194/hess-22-6163-2018
https://doi.org/10.5194/hess-22-6163-2018
Review article
 | 
30 Nov 2018
Review article |  | 30 Nov 2018

Toward a conceptual framework of hyporheic exchange across spatial scales

Chiara Magliozzi, Robert C. Grabowski, Aaron I. Packman, and Stefan Krause

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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: 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
AR by Chiara Magliozzi on behalf of the Authors (29 Oct 2018)  Manuscript 
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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.