Articles | Volume 22, issue 1
https://doi.org/10.5194/hess-22-509-2018
https://doi.org/10.5194/hess-22-509-2018
Research article
 | 
22 Jan 2018
Research article |  | 22 Jan 2018

Temperature signal in suspended sediment export from an Alpine catchment

Anna Costa, Peter Molnar, Laura Stutenbecker, Maarten Bakker, Tiago A. Silva, Fritz Schlunegger, Stuart N. Lane, Jean-Luc Loizeau, and Stéphanie Girardclos

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by Editor and Referees) (28 Mar 2017) by Laurent Pfister
AR by Anna Costa on behalf of the Authors (08 Jun 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (02 Jul 2017) by Laurent Pfister
RR by Anonymous Referee #2 (07 Aug 2017)
ED: Publish subject to minor revisions (further review by Editor) (31 Aug 2017) by Laurent Pfister
AR by Anna Costa on behalf of the Authors (27 Sep 2017)  Author's response   Manuscript 
ED: Publish as is (05 Nov 2017) by Laurent Pfister
AR by Anna Costa on behalf of the Authors (15 Nov 2017)  Manuscript 
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Short summary
We explore the signal of a warmer climate in the suspended-sediment dynamics of a regulated and human-impacted Alpine catchment. We demonstrate that temperature-driven enhanced melting of glaciers, which occurred in the mid-1980s, played a dominant role in suspended sediment concentration rise, through increased runoff from sediment-rich proglacial areas, increased contribution of sediment-rich meltwater, and increased sediment supply in proglacial areas due to glacier recession.