about
Converging flow and anisotropy cause large-scale folding in Greenland's ice sheetBrief Communication: Newly developing rift in Larsen C Ice Shelf presents significant risk to stabilityPhysical analysis of an Antarctic ice core-towards an integration of micro- and macrodynamics of polar iceMarine ice regulates the future stability of a large Antarctic ice shelf.Massive subsurface ice formed by refreezing of ice-shelf melt pondsDynamic recrystallization during deformation of polycrystalline ice: insights from numerical simulations.Small-scale disturbances in the stratigraphy of the NEEM ice core: observations and numerical model simulationsStrain localization and dynamic recrystallization in the ice–air aggregate: a numerical studySurface melt and ponding on Larsen C Ice Shelf and the impact of föhn windsMarine ice formation in a suture zone on the Larsen C Ice Shelf and its influence on ice shelf dynamicsBasal crevasses in Larsen C Ice Shelf and implications for their global abundancePersistent iceberg groundings in the western Weddell Sea, AntarcticaPresent stability of the Larsen C ice shelf, Antarctic PeninsulaSurface structure and stability of the Larsen C ice shelf, Antarctic PeninsulaA consistent data set of Antarctic ice sheet topography, cavity geometry, and global bathymetryFull-field predictions of ice dynamic recrystallisation under simple shear conditionsInvestigating englacial reflections with vibro- and explosive-seismic surveys at Halvfarryggen ice dome, Antarctica
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P50
description
hulumtuese
@sq
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Daniela Jansen
@ast
Daniela Jansen
@en
Daniela Jansen
@es
Daniela Jansen
@nl
Daniela Jansen
@sl
type
label
Daniela Jansen
@ast
Daniela Jansen
@en
Daniela Jansen
@es
Daniela Jansen
@nl
Daniela Jansen
@sl
prefLabel
Daniela Jansen
@ast
Daniela Jansen
@en
Daniela Jansen
@es
Daniela Jansen
@nl
Daniela Jansen
@sl
P106
P1153
22937404100
P21
P31
P496
0000-0002-4412-5820