In: Oecologia, 2015, vol. 179, no. 3, p. 765-775
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In: The Astronomy and Astrophysics Review, 2015, vol. 23, no. 1, p. 1-98
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In: Nature, 2019, vol. 573, no. 7774, p. 403–407
In recent decades, meltwater runoff has accelerated to become the dominant mechanism for mass loss in the Greenland ice sheet1,2,3. In Greenland’s high- elevation interior, porous snow and firn accumulate; these can absorb surface meltwater and inhibit runoff4, but this buffering effect is limited if enough water refreezes near the surface to restrict percolation5,6. However, the influence...
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In: Frontiers in Earth Science, 2018, vol. 6, p. -
The surface snow density of glaciers and ice sheets is of fundamental importance in converting volume to mass in both altimetry and surface mass balance studies, yet it is often poorly constrained. Site-specific surface snow densities are typically derived from empirical relations based on temperature and wind speed. These parameterizations commonly calculate the average density of the top...
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In: The Astronomy and Astrophysics Review, 2009, vol. 17, no. 3, p. 309-408
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