Mathematical modelling of subglacial drainage and erosion
The classical theory of channelized subglacial drainage,due orginally to Röthlisberger (1972) and Nye (1976), considers water flow in an ice channel overlying a rigid, impermeable bed. At steady flow, creep closure of the channel walls is counteracted by melt-back due to heat dissipation, and this l...
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| フォーマット: | 学位論文 |
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University of Oxford
1998
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