Articles | Volume 4, issue 1
https://doi.org/10.5194/tc-4-13-2010
https://doi.org/10.5194/tc-4-13-2010
15 Jan 2010
 | 15 Jan 2010

Reduced glacier sliding caused by persistent drainage from a subglacial lake

E. Magnússon, H. Björnsson, H. Rott, and F. Pálsson

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Cited articles

Anderson, R. S., Walder, J. S., Anderson, S. P., Trabant, D. C., and Fountain, A. G.: The dynamic response of Kennicott Glacier, Alaska, USA, to the Hidden Creek Lake outburst flood, Ann. Glaciol., 40, 237–242, 2005.
Bacher, U., Bludovsky, S., Dorrer E., and Münzer, U.: Precision aerial survey of Vatnajökull, Iceland by digital photogrammetry, in: Proceedings of Third Turkish-German Joint Geodetic Days –Towards a Digital Age, edited by: Oltan, M. O. and Gründig, L., Istanbul Tech. Univ., Istanbul, 1–10, 1999.
Bartholomaus, T. C., Anderson, R. S., and Anderson, S. P.: Response of glacier motion to transient water storage, Nature Geosci., 1, 33–37, 2008.
Berthier, E., Björnsson, H., Pálsson, F., Feigl, K. L., Llubes, M., and Rémy, F.: The level of the Grimsvötn subglacial lake, Vatnajökull, Iceland, monitored with SPOT5 images, Earth Planet. Sc. Lett., 243, 293–302, 2006.
Björnsson, H.: Subglacial lakes and jökulhlaups in Iceland, Global Planet. Change, 35, 255–271, 2002.
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