Preprints
https://doi.org/10.5194/egusphere-2023-1928
https://doi.org/10.5194/egusphere-2023-1928
06 Sep 2023
 | 06 Sep 2023

Microstructure-based simulations of the viscous densification of snow and firn

Kévin Fourteau, Johannes Freitag, Mika Malinen, and Henning Löwe

Abstract. Accurate models for the viscous densification of snow and firn under mechanical stress are of primary importance for various applications, including avalanche prediction and the interpretation of ice cores. Formulations of snow and firn compaction in models are still largely empirical, instead of using microstructures from micro-computed tomography to numerically compute the mechanical behavior directly from the physics at the micro-scale. The main difficulty of the latter approach is the choice of the correct rheology/constitutive law governing the deformation of the ice matrix, which is still controversially discussed. Being aware of these uncertainties, we conducted a first systematic attempt of microstructure-based modeling of snow and firn compaction. We employed the Finite Element suite ElmerFEM using snow and firn microstructures from different sites in the Alps and Antarctica to explore which ice rheologies are able to reproduce observations. We thereby extended the ParStokes solver in ElmerFEM to facilitate parallel computing of transverse isotropic material laws for monocrystalline ice. We found that firn (density above 550 kg m-3) can be reasonably well simulated across different sites assuming a polycrystalline rheology (Glen's law) that is traditionally used in glacier or ice sheet modeling. In contrast, for snow (density below 550 kg m-3) the observations are in contradition with this rheology. To further comprehend this finding, we conducted a sensitivity study on different ice rheologies. None of the material models is able to explain the observed high compactive viscosity of depth hoar compared to rounded grains having the same density. While on one hand our results re-emphasize the limitations of our current mechanical understanding of the ice in snow, they constitute on the other hand a confirmation of the common picture of firn densification as a foam of polycrystalline ice through microstructure-based simulations.

Kévin Fourteau, Johannes Freitag, Mika Malinen, and Henning Löwe

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Kévin Fourteau, Johannes Freitag, Mika Malinen, and Henning Löwe
Kévin Fourteau, Johannes Freitag, Mika Malinen, and Henning Löwe

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Short summary
Understanding the settling of snow under its own weight has applications from avalanche forecast to ice core interpretation. We study how this settling can be modeled using 3D images of snow internal structure and ice deformation mechanics. We found that classical ice mechanics, as used for instance in glacier flow, explains the compaction of dense polar snow, but not that of lighter seasonal snow. How exactly the ice deforms during light snow compaction thus remains an open question.