Projecting Antarctic ice discharge using response functions from SeaRISE ice-sheet models

The largest uncertainty in projections of future sea-level change results from the potentially changing dynamical ice discharge from Antarctica. Basal ice-shelf melting induced by a warming ocean has been identified as a major cause for additional ice flow across the grounding line. Here we attempt...

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Bibliographic Details

Published in:	Earth System Dynamics
Main Authors:	A. Levermann, R. Winkelmann, S. Nowicki, J. L. Fastook, K. Frieler, R. Greve, H. H. Hellmer, M. A. Martin, M. Meinshausen, M. Mengel, A. J. Payne, D. Pollard, T. Sato, R. Timmermann, W. L. Wang, R. A. Bindschadler
Format:	Article
Language:	English
Published:	Copernicus Publications 2014-08-01
Subjects:	open climate campaign
Online Access:	http://www.earth-syst-dynam.net/5/271/2014/esd-5-271-2014.pdf