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

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...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Mikkelsen, Andreas Bech, Hubbard, Alun, MacFerrin, Mike, Box, Jason Eric, Doyle, Sam H., Fitzpatrick, Andrew, Hasholt, Bent, Bailey, Hannah L., Lindbäck, Katrin, Pettersson, Rickard
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-10-1147-2016
https://tc.copernicus.org/articles/10/1147/2016/