Numerical solution of moving boundary problems in glacier flow
Beside geographical and physical characteristics of the environment, mostly temperature changes drive glacier dynamical evolution with subglacial and supraglacial water release or approaching a metastable state. The appearance of subglacial lakes filling bedrock depressions, glacier sliding, crevasses formation and calving are linked climate change sensitive macro-phenomena, where interactions between the interfacing phases are crucial.
We shall discuss the mathematical modelling and the numerical simulation of one of the above glacier problems with moving boundary.
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