Growth and Thermal Structure of the Deep Ice in Byrd Land, Antarctica
Abstract Instead of starting with an initially dry, below sea-level basin undergoing glacierization, as was done in an earlier. model, the present computations are based on the existence of an open channel connecting the Ross and Bellingshausen Seas. The period of glacierization begins as the sea in...
| Published in: | Journal of Glaciology |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1961
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s0022143000017482 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017482 |