Modelling debris transport within glaciers by advection in a full-Stokes ice flow model
Glaciers with extensive surface debris cover respond differently to climate forcing than those without supraglacial debris. In order to include debris-covered glaciers in projections of glaciogenic runoff and sea level rise and to understand the paleoclimate proxy recorded by such glaciers, it i...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2018-01-01
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| Series: | The Cryosphere |
| Online Access: | https://www.the-cryosphere.net/12/189/2018/tc-12-189-2018.pdf |