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...
Autors principals: | Schoof, C, Hewitt, I, Werder, M |
---|---|
Format: | Journal article |
Idioma: | English |
Publicat: |
2012
|
Ítems similars
-
Flotation and free surface flow in a model for subglacial drainage. Part 2. Channel flow
per: Hewitt, I, et al.
Publicat: (2012) -
Modelling distributed and channelized subglacial drainage: The spacing of channels
per: Hewitt, I
Publicat: (2011) -
Oscillatory subglacial drainage in the absence of surface melt
per: C. Schoof, et al.
Publicat: (2014-05-01) -
Modeling Antarctic subglacial lake filling and drainage cycles
per: C. F. Dow, et al.
Publicat: (2016-07-01) -
Improved representation of laminar and turbulent sheet flow in subglacial drainage models
per: Tim Hill, et al.
Publicat: (2024-01-01)