David Lilien
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Accelerating ice flow at the onset of the Northeast Greenland Ice Stream
Crystal fabric anisotropy causes directional hardening of the Northeast Greenland Ice Stream
On the Limitations of Using Polarimetric Radar Sounding to Infer the Crystal Orientation Fabric of Ice Masses
Modeling Ice-Crystal Fabric as a Proxy for Ice-Stream Stability
Brief Communication: New radar constraints support presence of ice older than 1.5 Myr at Little Dome C
Effect of an orientation-dependent non-linear grain fluidity on bulk directional enhancement factors
Modeling ice-crystal fabric as a proxy for ice-stream stability
Modeling fabric development using coupled non-parametric orientation and lattice strain-energy distribution functions
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