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Modelling seasonal meltwater forcing of the velocity of land-terminating margins of the Greenland Ice Sheet
Surface runoff at the margin of the Greenland Ice Sheet (GrIS) drains to the ice-sheet bed, leading to enhanced summer ice flow. Ice velocities show a pattern of early summer acceleration followed by mid-summer deceleration due to evolution of the subglacial hydrology system in response to meltw...
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Autores principales: | , |
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Formato: | Artigo |
Lenguaje: | Inglês |
Publicado: |
Copernicus Publications
2018-03-01
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Colección: | The Cryosphere |
Acceso en línea: | https://www.the-cryosphere.net/12/971/2018/tc-12-971-2018.pdf |
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