Fig. 2: Modelled subglacial channel discharge from paleo, modern, and future time snapshots.
From: The past, present, and future evolution of Aurora Subglacial Basin’s subglacial drainage system
Panels show the channel discharge under grounded ice at a the Eocene–Oligocene Boundary; b the Mid-Miocene; c present day; d 2100 CE, under maximum volumes of ice loss; and e 2100 CE under maximum volumes of ice gain. Black lines show the grounding lines, where water exits the domain, for each simulation. Dotted lines and abbreviations point to glacier locations. B Bond Glacier, MU Moscow University Ice Shelf, T Totten Glacier, V Vanderford Glacier. Channel discharge for each glacier labelled in the figure panels at each time snapshot is included in the supplementary material (Figs. S8–S12). Source data are provided as a Source data file.
