a) Locations of firn surveys conducted at NEGIS around the EGRIP

Survey area at the NEGIS showing (a) along‐ and (c) across‐flow

Fraction of initial ice thickness f (colorbar) in the vicinity of the

Shear margins in upper half of Northeast Greenland Ice Stream were established two millennia ago

Overview of input parameters and simulation results of the outlet NEGIS

Time evolution of the cumulative flux response number, cFRN (Eq. 1)

Shear margins in upper half of Northeast Greenland Ice Stream were established two millennia ago

Wet subglacial bedforms of the NE Greenland Ice Stream shear margins, Annals of Glaciology

Overview of input parameters and simulation results of the outlet NEGIS

PDF) Modeling enhanced firn densification due to strain softening

Bed topography and subglacial landforms in the onset region of the Northeast Greenland Ice Stream, Annals of Glaciology

Enhanced Firn Densification in High‐Accumulation Shear Margins of the NE Greenland Ice Stream - Riverman - 2019 - Journal of Geophysical Research: Earth Surface - Wiley Online Library

Difference of surface velocity v FS−BP-like s = v FS s − v BP-like s

TC - Modeling enhanced firn densification due to strain softening