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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Cited articles

Abermann, J., Kinnard, C., and MacDonell, S.: Albedo variations and the impact of clouds on glaciers in the Chilean semi-arid Andes J. Glaciol., 60, 183–191, 2014. 
Adhikari, S. and Marshall, S. J.: Influence of high-order mechanics on simulation of glacier response to climate change: insights from Haig Glacier, Canadian Rocky Mountains, The Cryosphere, 7, 1527–1541, https://doi.org/10.5194/tc-7-1527-2013, 2013. 
Andreas, E. L.: Parameterizing scalar transfer over snow and ice: a review, J. Hydrometeorol., 3, 417–432, 2002. 
Aoki, T., Kuchiki, K., Niwano, M., Kodama Y., Hosaka M., and Tanaka, T.: Physically based snow albedo model for calculating broadband albedos and the solar heating profile in snowpack for general circulation models, J. Geophys. Res., 116, D11114, https://doi.org/10.1029/2010JD015507, 2011. 
Arendt, A. and Sharp, M. J.: Energy balance measurements on a Canadian high Arctic glacier and their implications for mass balance modelling, IAHS Publ. 256, Symposium at Birmingham, 1 July 1999 – Interactions between the Cryosphere, Climate and Greenhouse Gases, 165–172, 1999. 
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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.