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 equili...
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| Principais autores: | , , , , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Copernicus Publications
2016-05-01
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| coleção: | The Cryosphere |
| Acesso em linha: | http://www.the-cryosphere.net/10/1147/2016/tc-10-1147-2016.pdf |
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