Flotation and free surface flow in a model for subglacial drainage. Part 1. Distributed drainage
We present a continuum model for melt water drainage through a spatially distributed system of connected subglacial cavities, and consider in this context the complications introduced when effective pressure or water pressure drops to zero. Instead of unphysically allowing water pressure to become n...
主要な著者: | Schoof, C, Hewitt, I, Werder, M |
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フォーマット: | Journal article |
言語: | English |
出版事項: |
2012
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