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Published byJosephine Turner Modified over 9 years ago
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Simulation of Snow Metamorphism Pedro Rodriguez
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Method Part 1: Constructing a snowpack Bi-continuous Model: summation of randomized cosine vectors + cutoff Part 2: Mass Transfer by Temperature Gradient Fick Flow drives mass transfer In simulation, empirical mass transfer used Particles sublimated, then deposited Run ‘main.m’
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Movies
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References “Dissertation: The thermophysical and microstructural effects of an artificial ice layer in natural snow under kinetic growth metamorphism”, Ethan Greene “The formation rate of depth hoar”, J.C. Giddings “Model for dry snow metamorphism by interparticle vapor flux”, H. Gubler “Theory of metamorphism of dry snow”, S. C. Colbeck “On heat and mass flux through dry snow”, E. Palm and M. Tveitereid “Water vapor transport in snow: a 2-d simulation of temperature gradient metamorphism”, M. Christon et all “Electromagnetic models of co/cross polarization of bictontinuous/dmrt in radar remote sensing of terrestrial snow at X- and Ku-band for CoReH2O and SCLP Applications”, X. Xu, L. Tsang
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