Mathematical models of glacier sliding and drumlin formation
One of the central difficulties in many models of glacier and ice sheet flow lies in the prescription of boundary conditions at the bed. Often, processes which occur there dominate the evolution of the ice mass as they control the speed at which the ice is able to slide over the bed. In part I of th...
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| Materiálatiipa: | Oahppočájánas |
| Almmustuhtton: |
University of Oxford;Mathematical Institute
2002
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