On the transport of moisture in polythermal glaciers
From MaRDI portal
Publication:4726000
DOI10.1080/03091928408222846zbMath0616.76118OpenAlexW2101438228WikidataQ114640530 ScholiaQ114640530MaRDI QIDQ4726000
Publication date: 1984
Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1080/03091928408222846
well-posednessDarcy's lawconstitutive lawenergy equationtwo-phase flow modelmelting temperaturepolythermal glaciers'porous' geometryice-water mixturemechanical constitutive relationmoisture fluxtemperature zone
Related Items (10)
A cell-centered finite difference method for a degenerate elliptic equation arising from two-phase mixtures ⋮ A model for polythermal ice incorporating gravity-driven moisture transport ⋮ A hybridized discontinuous Galerkin method for a linear degenerate elliptic equation arising from two-phase mixtures ⋮ Implicit solitary wave solutions of the generalized magma equation ⋮ A nonequilibrium theory of a slurry ⋮ Mixed Methods for Two-Phase Darcy--Stokes Mixtures of Partially Melted Materials with Regions of Zero Porosity ⋮ A model for the spreading and compaction of two-phase viscous gravity currents ⋮ A Linear Degenerate Elliptic Equation Arising from Two-Phase Mixtures ⋮ A mathematical model of magma transport in the asthenosphere ⋮ Water transport in planetary ice shells by two-phase flow – a parametric study
Cites Work
- Unnamed Item
- Unnamed Item
- Conduit flow of a fluid through its solid phase and its application to intraglacial channel flow
- A mathematical model of polythermal glaciers and ice sheets
- Spatial averaging in the mechanics of heterogeneous and dispersed systems
- The Stefan Problem: Comments on its Present State
- A theoretical treatment of the sliding of glaciers in the absense of cavitation
- The influence of interfacial pressure forces on the character of two-phase flow model equations
This page was built for publication: On the transport of moisture in polythermal glaciers
