The mathematical modelling for studying the evolution of a grounded temperate icefield flowing from an ice divide is detailed. The conjecture of the existence of a subglacial lake is considered, in particular regarding the influence of physical and geometrical parameters.
Diagnostic simulation of a subglacial lake at Amundsenisen (South-Spitzbergen). Part 1: a mathematical model.
Daniela Mansutti;
2011
Abstract
The mathematical modelling for studying the evolution of a grounded temperate icefield flowing from an ice divide is detailed. The conjecture of the existence of a subglacial lake is considered, in particular regarding the influence of physical and geometrical parameters.File in questo prodotto:
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