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Local topography increasingly influences the mass balance of a retreating cirque glacier

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Figure

Figure 1. (a) Study area in the US Northern Rocky Mountains, lo-cated just south of the USA–Canada border, as indicated by thered box on the inset map
Figure 2. Sperry Glacier on 1 September 2009. Arrow points tothe north. Note low-sloping proglacial terrain
Figure 3. Elevation change over Sperry Glacier from (a, b) 1950 to 1960, (c, d) 1960 to 2005, and (e, f) 2005 to 2014
Table 1. Area-averaged glaciological mass balance values used inthis study. Winter balances are as reported by Clark et al
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