Ice-shelf vibrations modeled by a full 3-D elastic model
Forced ice-shelf vibration modeling is performed using a full 3-D finite-difference elastic model, which also takes into account sub-ice seawater flow. The sea water flow is described by the wave equation. Ice-shelf flexure therefore results from hydrostatic pressure perturbations in the sub-ice sea...
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| Format: | Article |
| Language: | English |
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Cambridge University Press
2019-09-01
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| Series: | Annals of Glaciology |
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| Online Access: | https://www.cambridge.org/core/product/identifier/S0260305519000090/type/journal_article |