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....
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| Format: | Article |
| Language: | English |
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MDPI AG
2018-12-01
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| Series: | Geosciences |
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| Online Access: | https://www.mdpi.com/2076-3263/8/12/464 |