Modeling Dry-Snow Densification without Abrupt Transition
An empirical model for the densification of dry snow has been calibrated using strain-rate data from Pine Island Glacier basin, Antarctica. The model provides for a smooth transition between Stage 1 and Stage 2 densification, and leads to an analytical expression for density as a function of depth....
Published in: | Geosciences |
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Format: | Text |
Language: | English |
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Multidisciplinary Digital Publishing Institute
2018
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Online Access: | https://doi.org/10.3390/geosciences8120464 |