Shaw TE, Ulloa G, Farías Barahona D, Fernandez R, Lattus JM, McPhee J (2021)
Publication Type: Journal article
Publication year: 2021
Book Volume: 67
Pages Range: 158-169
Journal Issue: 261
DOI: 10.1017/jog.2020.102
Surface albedo typically dominates the mass balance of mountain glaciers, though long-Term trends and patterns of glacier albedo are seldom explored. We calculated broadband shortwave albedo for glaciers in the central Chilean Andes (33-34°S) using end-of-summer Landsat scenes between 1986 and 2020. We found a high inter-Annual variability of glacier-wide albedo that is largely a function of the glacier fractional snow-covered area and the total precipitation of the preceding hydrological year (up to 69% of the inter-Annual variance explained). Under the 2010-2020 'Mega Drought' period, the mean albedo, regionally averaged ranging from 0.25-0.5, decreased by-0.05 on average relative to 1986-2009, with the greatest reduction occurring 3500-5000 m a.s.l. In 2020, differences relative to 1986-2009 were-0.14 on average as a result of near-complete absence of late summer snow cover and the driest hydrological year since the Landsat observation period began (90% reduction of annual precipitation relative to the 1986-2009 period). We found statistically significant, negative trends in glacier ice albedo of up to-0.03 per decade, a trend that would have serious implications for the future water security of the region, because glacier ice melt acts to buffer streamflow shortages under severe drought conditions.
APA:
Shaw, T.E., Ulloa, G., Farías Barahona, D., Fernandez, R., Lattus, J.M., & McPhee, J. (2021). Glacier albedo reduction and drought effects in the extratropical Andes, 1986-2020. Journal of Glaciology, 67(261), 158-169. https://dx.doi.org/10.1017/jog.2020.102
MLA:
Shaw, Thomas E., et al. "Glacier albedo reduction and drought effects in the extratropical Andes, 1986-2020." Journal of Glaciology 67.261 (2021): 158-169.
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