Abstract
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Momentum, mass and energy balance laws provide the tools for the study of the evolution of an icefield covering a subglacial lake. The ice is described as a non-Newtonian fluid with a power-law constitutive relationship with temperature- and stress-dependent viscosity (Glen?s law) [1]. The phase transition mechanisms at the air/ice and ice/water interfaces yield moving boundary formulations, and lake hydrodynamics requires equation reduction for treating the turbulence. | |
International
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Si |
Congress
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Congreso de Métodos Numéricos en Ingeniería CMN 2013, |
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960 |
Place
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Bilbao, España |
Reviewers
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Si |
ISBN/ISSN
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978-84-941531-4-3 |
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Start Date
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25/07/2013 |
End Date
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28/07/2013 |
From page
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771 |
To page
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771 |
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Congreso de Métodos Numéricos en Ingeniería CMN 2013, 25-28 Junio 2013, Bilbao, España. International Center for Numerical Methods in Engineering (CIMNE), Barcelona, España, 2013, |