Articles | Volume 21, issue 7
https://doi.org/10.5194/hess-21-3249-2017
https://doi.org/10.5194/hess-21-3249-2017
Research article
 | 
03 Jul 2017
Research article |  | 03 Jul 2017

Assessing glacier melt contribution to streamflow at Universidad Glacier, central Andes of Chile

Claudio Bravo, Thomas Loriaux, Andrés Rivera, and Ben W. Brock

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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) (15 Jan 2017) by Jan Seibert
AR by Claudio Bravo on behalf of the Authors (21 Feb 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (21 Feb 2017) by Jan Seibert
RR by Anonymous Referee #1 (23 Mar 2017)
RR by Anonymous Referee #2 (03 Apr 2017)
ED: Reconsider after major revisions (further review by Editor and Referees) (04 Apr 2017) by Jan Seibert
AR by Claudio Bravo on behalf of the Authors (28 Apr 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (02 May 2017) by Jan Seibert
RR by Anonymous Referee #2 (18 May 2017)
ED: Publish subject to minor revisions (further review by Editor) (20 May 2017) by Jan Seibert
AR by Claudio Bravo on behalf of the Authors (26 May 2017)  Author's response    Manuscript
ED: Publish subject to technical corrections (30 May 2017) by Jan Seibert
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Short summary
We present an analysis of meteorological conditions and melt for Universidad Glacier in central Chile. This glacier is characterized by high melt rates over the ablation season, representing a mean contribution of between 10 and 13 % of the total runoff observed in the upper Tinguiririca Basin during the November 2009 to March 2010 period. Few studies have quantified the glacier melt contribution to river runoff in Chile, and this work represents a new precedent for the Andes.