Interpreting englacial layer deformation in the presence of complex ice flow history with synthetic radargrams
Fast ice flow on the Antarctic continent constitutes much of the mass loss from the ice sheet. However, geophysical methods struggle to constrain ice flow history at depth, or separate the signatures of topography, ice dynamics and basal conditions on layer structure. We develop and demonstrate a me...
Kaydedildi:
| Asıl Yazarlar: | , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Cambridge University Press
2020-04-01
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| Seri Bilgileri: | Annals of Glaciology |
| Konular: | |
| Online Erişim: | https://www.cambridge.org/core/product/identifier/S0260305519000417/type/journal_article |
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