activity
20092015
most citedContinuum-mechanical, Anisotropic Flow model for polar ice masses, based on an anisotropic Flow Enhancement factor

77 citations · 179 across the 8 of their papers we have counts for

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Showing 2009Show all

6 papers · 1 filter

physics.geo-ph2009

Decay of the Greenland Ice Sheet due to surface-meltwater-induced acceleration of basal sliding

Ralf Greve, Shin Sugiyama

Simulations of the Greenland Ice Sheet are carried out with a high-resolution version of the ice-sheet model SICOPOLIS for several global-warming scenarios for the period 1990-2350…

physics.geo-ph2009★ 6 cited

Fluid dynamics of planetary ices

Ralf Greve

The role of water ice in the solar system is reviewed from a fluid-dynamical point of view. On Earth and Mars, water ice forms ice sheets, ice caps and glaciers at the surface, whi…

physics.geo-ph2009★ 1 cited

A continuum-mechanical model for the flow of anisotropic polar ice

Ralf Greve, Luca Placidi, Hakime Seddik

In order to study the mechanical behaviour of polar ice masses, the method of continuum mechanics is used. The newly developed CAFFE model (Continuum-mechanical, Anisotropic Flow m…

physics.geo-ph2009★ 23 cited

MAIC-2, a latitudinal model for the Martian surface temperature, atmospheric water transport and surface glaciation

Ralf Greve, Bjoern Grieger, Oliver J. Stenzel

The Mars Atmosphere-Ice Coupler MAIC-2 is a simple, latitudinal model, which consists of a set of parameterisations for the surface temperature, the atmospheric water transport and…

physics.geo-ph2009★ 77 cited

Continuum-mechanical, Anisotropic Flow model for polar ice masses, based on an anisotropic Flow Enhancement factor

Luca Placidi, Ralf Greve, Hakime Seddik +1

A complete theoretical presentation of the Continuum-mechanical, Anisotropic Flow model, based on an anisotropic Flow Enhancement factor (CAFFE model) is given. The CAFFE model is…

physics.geo-ph2009★ 19 cited

Numerical simulation of the evolution of glacial valley cross sections

Hakime Seddik, Ralf Greve, Shin Sugiyama +1

A numerical model was developed for simulating the formation of U-shaped glacial valleys by coupling a two-dimensional ice flow model with an erosion model for a transverse cross s…