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Modelling ice-divide dynamics by perturbation methods methods, when the ice creep is described by Glen's flow law. This approach allows us to model the ice
Dependence of sea ice yield-curve shape on ice thicknessIn this note, the authors discuss the contribution that frictional sliding of ice floes (or floe
Bubbly-ice densification in ice sheets: I. TheoryDry snow on the surface of polar ice ice sheets is first densified and metamorphosed to produce
Anisotropic model for granulated sea ice dynamicsA continuum model describing sea ice as a layer of granulated thick ice, consisting of many rigid
Modelling the rheology of sea ice as a collection of diamond-shaped floesIn polar oceans, seawater freezes to form a layer of sea ice of several metres thickness that can
Bubbly-ice densification in ice sheets: I. TheoryDry snow on the surface of polar ice ice sheets is first densified and metamorphosed to produce
A continuum anisotropic model of sea-ice dynamicsWe develop the essential ingredients of a new, continuum and anisotropic model of sea-ice dynamics
Anisotropic model for granulated sea ice dynamicsA continuum model describing sea ice as a layer of granulated thick ice, consisting of many rigid
Ice sheet modelling taking account of glacier ice compressibility and mass transfer processes in ice sheets with allowance for compressibility effects. -K.Clayton
Modelling ice-divide dynamics by perturbation methods methods, when the ice creep is described by Glen's flow law. This approach allows us to model the ice
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