Modelling lateral meltwater flow and superimposed ice formation atop Greenland's near-surface ice slabs
At high elevations on the Greenland ice sheet meltwater percolates and refreezes in place, and hence does not contribute to mass loss. However, meltwater generation and associated surface runoff is occurring from increasingly higher altitudes, causing changes in firn stratigraphy that have led to th...
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| Hauptverfasser: | , , , |
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| Format: | Artigo |
| Sprache: | Inglês |
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Cambridge University Press
2024-01-01
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| Schriftenreihe: | Journal of Glaciology |
| Schlagworte: | |
| Online-Zugang: | https://www.cambridge.org/core/product/identifier/S0022143024000698/type/journal_article |
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