A phase-field model for wet snow metamorphism
Adrian Moure, Xiaojing Fu

TL;DR
This paper introduces a pore-scale phase-field model for wet snow metamorphism, capturing phase transitions among ice, water vapor, and liquid water, and analyzing how humidity and temperature influence snow microstructure evolution.
Contribution
The novel phase-field model simultaneously simulates sublimation, evaporation, and melting in wet snow, providing detailed insights into microstructural changes at the pore scale.
Findings
Humidity and temperature significantly affect snow metamorphism dynamics.
Liquid melt content influences the transition processes before percolation.
The model can be extended to study water phase transitions in other systems.
Abstract
The microstructure of snow determines its fundamental properties such as the mechanical strength, reflectivity, or the thermo-hydraulic properties. Snow undergoes continuous microstructural changes due to local gradients in temperature, humidity or curvature, in a process known as snow metamorphism. In this work, we focus on wet snow metamorphism, which occurs when temperature is close to the melting point and involves phase transitions amongst liquid water, water vapor, and solid ice. We propose a pore-scale phase-field model that simultaneously captures the three relevant phase-change phenomena: sublimation (deposition), evaporation (condensation), and melting (solidification). The phase-field formulation allows one to track the temperature evolution amongst the three phases and the water vapor concentration in the air. Our three-phase model recovers the corresponding two-phase…
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Taxonomy
TopicsSolidification and crystal growth phenomena · Advanced Mathematical Modeling in Engineering · Arctic and Antarctic ice dynamics
