Dynamics of ice shelves and their sensitivity to changing mass-balance quantities Model results for Filchner-Ronne ice shelf, Antarctica
Previous evidence suggests basal layer up to 400 m thick. Attempts to demonstrate that this consists of marine ice which grew in water column beneath ice shelf. Application of finite-differences ice-flow model reveals contribution of bottom melting and accumulation to mass budget. Basal interactions...
| Main Authors: | , |
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
1990
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| Subjects: | |
| Online Access: | https://epic.awi.de/id/eprint/593/ https://hdl.handle.net/10013/epic.11180 |