Increasing contribution of grain boundary compliance to polycrystalline ice elasticity as temperature increases
Measured elastic stiffnesses of ice polycrystals decrease with increasing temperature due to a decrease in grain boundary stiffness with increasing temperature. In this paper, we represent grain boundaries as imperfectly bonded interfaces, across which traction is continuous, but displacement may be...
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| Format: | Article |
| Language: | English |
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Cambridge University Press
2018-08-01
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| Series: | Journal of Glaciology |
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| Online Access: | https://www.cambridge.org/core/product/identifier/S0022143018000564/type/journal_article |