Extraordinary runoff from the Greenland ice sheet in 2012 amplified by hypsometry and depleted firn retention

• Published in: The Cryosphere
• Main Authors: A. B. Mikkelsen, A. Hubbard, M. MacFerrin, J. E. Box, S. H. Doyle, A. Fitzpatrick, B. Hasholt, H. L. Bailey, K. Lindbäck, R. Pettersson
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2016
• Subjects: Environmental sciences; GE1-350; Geology; QE1-996.5; Greenland; Kangerlussuaq; Harper; Ice Sheet; The Cryosphere
• Online Access: https://doi.org/10.5194/tc-10-1147-2016; https://doaj.org/article/1ea249cbde1e4ff6ae1e2dd49d56b169

It has been argued that the infiltration and retention of meltwater within firn across the percolation zone of the Greenland ice sheet has the potential to buffer up to ∼ 3.6 mm of global sea-level rise (Harper et al., 2012). Despite evidence confirming active refreezing processes above the equilibr...