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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 7, issue 2
The Cryosphere, 7, 407–417, 2013
https://doi.org/10.5194/tc-7-407-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 7, 407–417, 2013
https://doi.org/10.5194/tc-7-407-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 01 Mar 2013

Research article | 01 Mar 2013

Surface undulations of Antarctic ice streams tightly controlled by bedrock topography

J. De Rydt et al.

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Cited articles

Arthern, R. J. and Gudmundsson, G. H.. Initialization of ice-sheet forecasts viewed as an inverse Robin problem, J. Glaciol., 560, 527–533, 2010.
Bamber, J. L.,Vaughan, D. G. , and Joughin, I.: Widespread complex flow in the interior of the Antarctic ice sheet, Science, 2870, 1248–1250, 2000.
Budd, W. F.: Ice flow over bedrock perturbations, J. Glaciol., 90, 29–48, 1970.
Corr, H. F. J., Ferraccioli, F., Frearson, N., Jordan, T., Robinson, C., Armadillo, E., Caneva, G., Bozzo, E., and Tabacco, I.: Airborne radio-echo sounding of the Wilkes Subglacial Basin, the Transantarctic Mountains, and the Dome C region, Terra Ant. Reports, 13, 55–63, 2007.
Cuffey, K. M. and Paterson, W. S. B.: The Physics of Glaciers, 4th Edn., Elsevier, Burlington, USA, 2010.
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