Articles | Volume 14, issue 10
https://doi.org/10.5194/tc-14-3249-2020
https://doi.org/10.5194/tc-14-3249-2020
Research article
 | 
02 Oct 2020
Research article |  | 02 Oct 2020

Seasonal and interannual variability of melt-season albedo at Haig Glacier, Canadian Rocky Mountains

Shawn J. Marshall and Kristina Miller

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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) (19 Jul 2020) by Valentina Radic
AR by Shawn Marshall on behalf of the Authors (19 Jul 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (04 Aug 2020) by Valentina Radic
RR by Anonymous Referee #2 (05 Aug 2020)
ED: Publish as is (13 Aug 2020) by Valentina Radic
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Short summary
Surface-albedo measurements from 2002 to 2017 from Haig Glacier in the Canadian Rockies provide no evidence of long-term trends (i.e., the glacier does not appear to be darkening), but there are large variations in albedo over the melt season and from year to year. The glacier ice is exceptionally dark in association with forest fire fallout but is effectively cleansed by meltwater or rainfall. Summer snowfall plays an important role in refreshing the glacier surface and reducing summer melt.