UB Paderborn / Katalog / Suche / in CDI

Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences, 1997-05, Vol.355 (1726), p.921-974

Greve, Ralf

1997

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Studies on the variability of the Greenland Ice Sheet and climate

Polar science, 2021-03, Vol.27, p.100557, Article 100557

2021

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

Continuum mechanics and thermodynamics, 2010-03, Vol.22 (3), p.221-237

2010

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Computational modeling of flow-induced anisotropy of polar ice for the EDML deep drilling site, Antarctica: The effect of rotation recrystallization and grain boundary migration

International journal for numerical and analytical methods in geomechanics, 2012-05, Vol.36 (7), p.892-917

2012

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A full Stokes-flow thermo-mechanical model for firn and ice applied to the Gorshkov crater glacier, Kamchatka

Annals of glaciology, 2007-01, Vol.45 (1), p.29-37

2007

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Large-scale instabilities of the Laurentide ice sheet simulated in a fully coupled climate-system model

Geophysical research letters, 2002-12, Vol.29 (24), p.69-1-69-4

2002

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Application of a continuum-mechanical model for the flow of anisotropic polar ice to the EDML core, Antarctica

Journal of glaciology, 2008-01, Vol.54 (187), p.631-642

2008

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Results from the Ice-Sheet Model Intercomparison Project–Heinrich Event Intercomparison (ISMIP HEINO)

Journal of glaciology, 2010-01, Vol.56 (197), p.371-383

2010

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Mass loss of the Greenland ice sheet until the year 3000 under a sustained late-21st-century climate

Coupled simulations of Greenland Ice Sheet and climate change up to A.D. 2300

Relation of measured basal temperatures and the spatial distribution of the geothermal heat flux for the Greenland ice sheet

Mass loss of the Antarctic ice sheet until the year 3000 under a sustained late-21st-century climate

Future projections for the Antarctic ice sheet until the year 2300 with a climate-index method

Response of the flow dynamics of Bowdoin Glacier, northwestern Greenland, to basal lubrication and tidal forcing

Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet

Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting

Comparison of thermodynamics solvers in the polythermal ice sheet model SICOPOLIS

Possible impacts of a 1000 km long hypothetical subglacial river valley towards Petermann Glacier in northern Greenland

Application of a Polythermal Three-Dimensional Ice Sheet Model to the Greenland Ice Sheet: Response to Steady-State and Transient Climate Scenarios

Constraining the geothermal heat flux in Greenland at regions of radar-detected basal water

Resolution of ice streams and outlet glaciers in large-scale simulations of the Greenland ice sheet

SICOPOLIS-AD v1: an open-source adjoint modeling framework for ice sheet simulation enabled by the algorithmic differentiation tool OpenAD

Transient simulation of the last glacial inception. Part I: glacial inception as a bifurcation in the climate system

Paleoglaciological reconstructions for the Tibetan Plateau during the last glacial cycle: evaluating numerical ice sheet simulations driven by GCM-ensembles

On the pressure dependence of the rate factor in Glen’s flow law

A continuum–mechanical formulation for shallow polythermal ice sheets

Studies on the variability of the Greenland Ice Sheet and climate

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

Computational modeling of flow-induced anisotropy of polar ice for the EDML deep drilling site, Antarctica: The effect of rotation recrystallization and grain boundary migration

A full Stokes-flow thermo-mechanical model for firn and ice applied to the Gorshkov crater glacier, Kamchatka

Large-scale instabilities of the Laurentide ice sheet simulated in a fully coupled climate-system model

Application of a continuum-mechanical model for the flow of anisotropic polar ice to the EDML core, Antarctica

Results from the Ice-Sheet Model Intercomparison Project–Heinrich Event Intercomparison (ISMIP HEINO)

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