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Kinematic response of ice-rise divides to changes in ocean and atmosphere forcing

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Figure

Figure 1. (a) Location map of ice rises along the margin of the Antarctic ice sheet (Matsuoka et al., 2015)
Figure 2. Upper panel ((c)a–c) shows schematic (a) steady state, (b) divide migration induced by asymmetric surface mass balance forcing, and divide migration induced by ocean perturbation forcing
Table 1. Standard physical and numerical parameters used for thesimulations.
Figure 3. L-curve analysis to select Tikhonov parameters(b)(c) λB and λC: (a) 2-D cross section for variable λB and λC fixed at 107 Pa−2 m6 a−4
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