Change detection of bare-ice albedo in the Swiss Alps
Environmental sciences
QE1-996.5
13. Climate action
GE1-350
Geology
910 Geography & travel
15. Life on land
550 Earth sciences & geology
DOI:
10.5194/tc-13-397-2019
Publication Date:
2019-02-01T14:33:05Z
AUTHORS (3)
ABSTRACT
Abstract. Albedo feedback is an important driver of glacier melt
over bare-ice surfaces. Light-absorbing impurities strongly enhance glacier
melt rates but their abundance, composition and variations in space and time
are subject to considerable uncertainties and ongoing scientific debates. In
this study, we assess the temporal evolution of shortwave broadband albedo
derived from 15 end-of-summer Landsat scenes for the bare-ice areas of 39
large glaciers in the western and southern Swiss Alps. Trends in bare-ice
albedo crucially depend on the spatial scale considered. No significant
negative temporal trend in bare-ice albedo was found on a regional to
glacier-wide scale. However, at higher spatial scales, certain areas of
bare ice, including the lowermost elevations and margins of the ablation
zones,
revealed significant darkening over the study period 1999 to 2016. A total
glacier area of 13.5 km2 (equivalent to about 12 % of the average
end-of-summer bare-ice area in the study area) exhibited albedo trends
significant at the 95 % confidence level or higher. Most of this area was
affected by a negative albedo trend of about −0.05 decade−1. Generally,
bare-ice albedo exhibits a strong interannual variability, caused by a
complex interplay of meteorological conditions prior to the acquisition of
the data, local glacier characteristics and the date of the investigated
satellite imagery. Although a darkening of glacier ice was found to be
present over only a limited region, we emphasize that due to the recent and
projected growth of bare-ice areas and prolongation of the ablation season in
the region, the albedo feedback will considerably enhance the rate of glacier
mass loss in the Swiss Alps in the near future.
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