The Cryosphere Discuss., 5, 2035-2060, 2011
www.the-cryosphere-discuss.net/5/2035/2011/
doi:10.5194/tcd-5-2035-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal The Cryosphere (TC). Please refer to the corresponding final paper in TC.
Basal crevasses in Larsen C Ice Shelf and implications for their global abundance
A. Luckman1, D. Jansen1, B. Kulessa1, E. C. King2, P. Sammonds3, and D. I. Benn4,5
1School of the Environment and Society, Swansea University, UK
2British Antarctic Survey, High Cross, Cambridge, UK
3Department of Earth Sciences, University College London, UK
4University Centre in Svalbard, PO Box 156, 9171, Longyearbyen, Norway
5Department of Geography, University of St Andrews, UK

Abstract. Basal crevasses extend upwards from the base of ice bodies and can penetrate more than halfway through the ice column under conditions found commonly on ice shelves. As a result, they may locally modify the exchange of mass and energy between ice shelf and ocean, and by altering the shelf's mechanical properties could play a fundamental role in ice shelf stability. Although early studies revealed that such features may be abundant on Antarctic ice shelves, their geometrical properties and spatial distribution has gained little attention. We investigate basal crevasses in Larsen C Ice Shelf using field radar survey, remote sensing and numerical modelling. We demonstrate that a group of features visible in MODIS imagery are the surface expressions of basal crevasses in the form of surface troughs, and find that basal crevasses can be generated as a result of stresses well downstream of the grounding line. We show that linear elastic fracture mechanics modelling is a good predictor of basal crevasse penetration height where stresses are predominantly tensile, and that measured surface trough depth does not always reflect this height, probably because of snow accumulation in the trough, marine ice accretion in the crevasse, or stress bridging from the surrounding ice. We conclude that all features visible in MODIS imagery of ice shelves and previously labelled simply as "crevasses", where they are not full thickness rifts, must be basal crevasse troughs, highlighting a fundamental structural property of many ice shelves that may have been previously overlooked.

Citation: Luckman, A., Jansen, D., Kulessa, B., King, E. C., Sammonds, P., and Benn, D. I.: Basal crevasses in Larsen C Ice Shelf and implications for their global abundance, The Cryosphere Discuss., 5, 2035-2060, doi:10.5194/tcd-5-2035-2011, 2011.
 
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