Olaf Eisen
www.awi.de
0000-0002-6380-962X
Universität Bremen
112 papers found
Refreshing results…
Crystal orientation fabric anisotropy causes directional hardening of the Northeast Greenland Ice Stream
Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration
Investigating the Radar Response of Englacial Debris Entrained Basal Ice Units in East Antarctica Using Electromagnetic Forward Modeling
Holocene ice-stream shutdown and drainage basin reconfiguration in northeast Greenland
Predicting the steady-state isochronal stratigraphy of ice shelves using observations and modeling
Polarimetric radar reveals the spatial distribution of ice fabric at domes and divides in East Antarctica
Origin of englacial stratigraphy at three deep ice core sites of the Greenland Ice Sheet by synthetic radar modelling
Airborne ultra-wideband radar sounding over the shear margins and along flow lines at the onset region of the Northeast Greenland Ice Stream
Preserved landscapes underneath the Antarctic Ice Sheet reveal the geomorphological history of Jutulstraumen Basin
Investigating the internal structure of the Antarctic ice sheet: the utility of isochrones for spatiotemporal ice-sheet model calibration
Evidence for a grounding line fan at the onset of a basal channel under the ice shelf of Support Force Glacier, Antarctica, revealed by reflection seismics
The regional-scale surface mass balance of Pine Island Glacier, West Antarctica, over the period 2005–2014, derived from airborne radar soundings and neutron probe measurements
Antarctic Sedimentary Basins: defining crucial constraints on ice-sheet and solid-earth dynamic interactions
Investigating the internal structure of the Antarctic Ice Sheet: the utility of isochrones for spatio-temporal ice sheet model calibration
Interior of an ice stream: 3-D geometry of distorted radar stratigraphy of upstream NEGIS and vicinity.
Ice shelf internal reflection horizons reveal ice provenance, dynamics, surface accumulation and oceanic melt
Investigating seismic properties of the NEGIS onset region using ice-drilling noise as a seismic source
Fabric beats in radar data across the NEGIS ice stream
Polarimetric radar reveals the spatial distribution of ice fabric at domes in East Antarctica
Geophysics
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