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Projecting Antarctic ice discharge using response functions from SeaRISE ice-sheet models

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Figure

Figure 1. Schematic of procedure for the estimate of the uncertainty of the Antarctic dynamic contribution to future sea-level change
Figure 2. The four different basins for which ice-sheet responsefunctions are derived from the SeaRISE M2 experiments
Table 1. Mean depth of ice shelves in the different regions denotedin Fig. 2 as computed from Le Brocq et al
Figure 3. Linear response functions for the five ice-sheet models of Antarctica for each region as defined by Eq
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