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Simulating the Greenland ice sheet under present-day and palaeo constraints including a new discharge parameterization

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Figure

Figure 1. Principle sketch of the discharge parameterization overdicates the region over the ice sheet where the discharge parameter-ization applies
Figure 3. Simulated parameterized divergence of fast ice flow inm yr−1 (Eq. 3) at (a) present day and, (b) at Eemian from the modelversion with the most reduced Eemian ice sheet.
Figure 4. Error measures for a modelled ice sheet in the(c) {cd} × {cm} parameter space
Figure 5. Estimated constraints on the parameters(c)Eemian ice is simulated at the upstream position of NEEM are displayed in white.to sea-level rise between the Eemian and present day under our constraints
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