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In the context of global warming, the question of the stability of Antarctic ice shelves is critical for predicting any sea level rise. The behaviour of ice shelves is dependent on their boundary conditions. At the ice-ocean interface, these boundary conditions can be appraised by studying the properties of marine ice forming accretions at the base.
• F.R.S.-FNRS et Fonds associés (hors FRIA)
• PAI