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Past ice-sheet behaviour: retreat scenarios and changing controls in the Ross Sea, Antarctica

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Figure

Figure 1. Regional bathymetry of the Ross Sea continental shelfwith bed topography data acquired from BEDMAP2 (Fretwell etal., 2013)
Figure 2. Glacial geomorphic features of the continental shelf.meltwater channel in the Pennell Trough with complex channel morphology, associated with small-scale recessional ice-marginal features.(e)showing GZW (4b) in Glomar Challenger Basin modified fro
Fig. 3). This is consistent with previous interpretations of themaximum grounding line location (Licht et al., 1999; Shippet al., 1999)
Figure 4. Linear features in the eastern Ross Sea were grouped intoflow sets based on features mapped using multibeam data (solidlines) and interpolation between multibeam data (dotted lines)
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