Articles | Volume 27, issue 2
https://doi.org/10.5194/hess-27-543-2023
https://doi.org/10.5194/hess-27-543-2023
Research article
 | 
27 Jan 2023
Research article |  | 27 Jan 2023

Contribution of rock glacier discharge to late summer and fall streamflow in the Uinta Mountains, Utah, USA

Jeffrey S. Munroe and Alexander L. Handwerger

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (07 Nov 2022) by Günter Blöschl
AR by Jeffrey Munroe on behalf of the Authors (09 Nov 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (13 Nov 2022) by Günter Blöschl
RR by Anonymous Referee #2 (17 Dec 2022)
ED: Publish as is (29 Dec 2022) by Günter Blöschl
AR by Jeffrey Munroe on behalf of the Authors (02 Jan 2023)  Manuscript 
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Short summary
Rock glaciers are mixtures of ice and rock debris that are common landforms in high-mountain environments. We evaluated the role of rock glaciers as a component of mountain hydrology by collecting water samples during the summer and fall of 2021. Our results indicate that the water draining from rock glaciers late in the melt season is likely derived from old buried ice; they further demonstrate that this water collectively makes up about a quarter of streamflow during the month of September.