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Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting

Computer models are necessary for understanding and predicting marine ice sheet behaviour. However, there is uncertainty over implementation of physical processes at the ice base, both for grounded and floating glacial ice. Here we implement several sliding relations in a marine ice sheet flow-line...

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Auteurs principaux: R. M. Gladstone, R. C. Warner, B. K. Galton-Fenzi, O. Gagliardini, T. Zwinger, R. Greve
Format: Artigo
Langue:Inglês
Publié: Copernicus Publications 2017-01-01
Collection:The Cryosphere
Accès en ligne:http://www.the-cryosphere.net/11/319/2017/tc-11-319-2017.pdf
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