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Two independent methods for mapping the grounding line of an outlet glacier – an example from the Astrolabe Glacier, Terre Adélie, Antarctica

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Figure

Figure 1. Location of the Astrolabe Glacier in the Terre Adélie sector of East Antarctica from an Advanced Very High ResolutionRadiometer (AVHR) global picture (upper left)
Figure 3. Ice–ocean interactions near the grounding line. The top ofthe figure represents the grounded–floating transition for an outletglacier where hydrostatic equilibrium with a constant “non-tidal”ocean is assumed throughout
Figure 5. Ice–bedrock interface measured by GPR along profiles[QR] (A), [RU] (B) and [IJ] (C) of Fig
Figure 6. Theoretical hydrostatic floatation depth (blue curve witherror bars) computed with an ice density of 890 ± 10kg m−3 com-pared to the ice bottom depth (black curve) inferred from ground-penetrating radar operated from the ground
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