Articles | Volume 21, issue 7
https://doi.org/10.5194/hess-21-3727-2017
https://doi.org/10.5194/hess-21-3727-2017
Research article
 | 
21 Jul 2017
Research article |  | 21 Jul 2017

Form and function in hillslope hydrology: characterization of subsurface flow based on response observations

Lisa Angermann, Conrad Jackisch, Niklas Allroggen, Matthias Sprenger, Erwin Zehe, Jens Tronicke, Markus Weiler, and Theresa Blume

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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 (02 Sep 2016) by Ross Woods
AR by Lisa Angermann on behalf of the Authors (25 Nov 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (28 Nov 2016) by Ross Woods
RR by Anonymous Referee #2 (12 Jan 2017)
RR by Anonymous Referee #3 (18 Jan 2017)
ED: Publish subject to revisions (further review by Editor and Referees) (03 Feb 2017) by Ross Woods
AR by Lisa Angermann on behalf of the Authors (17 Mar 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (18 Mar 2017) by Ross Woods
RR by Anonymous Referee #3 (18 Apr 2017)
RR by Anonymous Referee #2 (18 Apr 2017)
ED: Publish subject to minor revisions (further review by Editor) (19 Apr 2017) by Ross Woods
AR by Lisa Angermann on behalf of the Authors (29 Apr 2017)  Author's response   Manuscript 
ED: Publish as is (22 May 2017) by Ross Woods
AR by Lisa Angermann on behalf of the Authors (01 Jun 2017)  Manuscript 
Short summary
This study investigates the temporal dynamics and response velocities of lateral preferential flow at the hillslope. The results are compared to catchment response behavior to infer the large-scale implications of the observed processes. A large portion of mobile water flows through preferential flow paths in the structured soils, causing an immediate discharge response. The study presents a methodological approach to cover the spatial and temporal domain of these highly heterogeneous processes.