Articles | Volume 23, issue 4
https://doi.org/10.5194/hess-23-2041-2019
https://doi.org/10.5194/hess-23-2041-2019
Research article
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24 Apr 2019
Research article | Highlight paper |  | 24 Apr 2019

Controls on spatial and temporal variability in streamflow and hydrochemistry in a glacierized catchment

Michael Engel, Daniele Penna, Giacomo Bertoldi, Gianluca Vignoli, Werner Tirler, and Francesco Comiti

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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) (02 Oct 2018) by Carlo De Michele
AR by Michael Engel on behalf of the Authors (13 Nov 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (25 Nov 2018) by Carlo De Michele
RR by Anonymous Referee #2 (11 Dec 2018)
RR by Anonymous Referee #3 (27 Feb 2019)
ED: Publish subject to minor revisions (review by editor) (09 Mar 2019) by Carlo De Michele
AR by Michael Engel on behalf of the Authors (26 Mar 2019)  Author's response   Manuscript 
ED: Publish as is (27 Mar 2019) by Carlo De Michele
AR by Michael Engel on behalf of the Authors (03 Apr 2019)
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Short summary
Hydrometric and geochemical dynamics are controlled by interplay of meteorological conditions, topography and geological heterogeneity. Nivo-meteorological indicators (such as global solar radiation, temperature and decreasing snow depth) explain monthly conductivity and isotopic dynamics best. These insights are important for better understanding hydrochemical responses of glacierized catchments under a changing cryosphere.