In: Environmental Management, 2015, vol. 55, no. 3, p. 536-549
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In: Theoretical and Applied Climatology, 2015, vol. 121, no. 1-2, p. 211-223
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In: Climate Dynamics, 2015, vol. 44, no. 7-8, p. 1857-1869
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In: The Cryosphere, 2020, vol. 14, no. 2, p. 521–538
One of the primary controls upon the melting of the Greenland Ice Sheet (GrIS) is albedo, a measure of how much solar radiation that hits a surface is reflected without being absorbed. Lower-albedo snow and ice surfaces therefore warm more quickly. There is a major difference in the albedo of snow-covered versus bare-ice surfaces, but observations also show that there is substantial spatio-...
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In: Journal of Mammary Gland Biology and Neoplasia, 2014, vol. 19, no. 1, p. 73-90
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