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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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Библиографические подробности
Главные авторы: C. P. Koziol, N. Arnold
Формат: Artigo
Язык:Inglês
Опубликовано: Copernicus Publications 2018-03-01
Серии:The Cryosphere
Online-ссылка:https://www.the-cryosphere.net/12/971/2018/tc-12-971-2018.pdf
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