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El desglaç a la base de Groenlàndia pot ser menor del que pensem
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Mechanical anisotropy: how do crystal-scale processes in rocks control large sca...
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Teaser POLARCSIC 360VR Ciencia en el Polo Sur
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Numerical modelling of polyphase deformation and recrystallization in polar firn...
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Fold and strain analysis of the large NE Greenland Ice Stream
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Deformation structures resulting from anisotropy during high-strain deformation...
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Dynamic recrystallisation of ice aggregates during co-axial viscoplastic deforma...
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FFT simulation of dynamic recrystallization in polar ice
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Strain localization and dynamic recrystallization in the ice–air aggregate: a nu...
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Computational analysis of dynamic recrystallization of ice aggregates during vis...
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Influence of initial preferred orientations on strain localisation and fold patt...
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Strain localization and dynamic recrystallization in the ice–air aggregate: a nu...
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Dynamic recrystallisation of ice aggregates during co-axial viscoplastic deforma...
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Band-pass-filtered ice-sheet surface elevation, thickness, velocity and derived...
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Greenland Ice Sheet - Higher non-linearity of ice flow significantly reduces est...
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Band-pass-filtered ice-sheet surface elevation, thickness, velocity and derived...
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Implications of air inclusions on ice microdynamics: Insights from numerical sim...
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The effect of melt on seismic anisotropy of ice polycrystalline aggregates
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Flow laws for ice sheet modelling: what do experiments tell us?
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Small scale folding observed in the NEEM ice core
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