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

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Academic year: 2017

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Table 1. Temperature values of the threshold of decay of the Greenland ice sheet for a number of valid model parameters.
Fig. 1. Principle sketch of the discharge parameterization over a part of the horizontal com- com-putational domain
Fig. 2. Distance field over the entire Greenland area in km. It is determined by the minimal distance of every land grid point (ice free and ice covered ones) to the coast (first ocean grid point, see Fig
Fig. 3. Simulated ice discharge measured in m yr −1 at (a) present-day and, (b) at Eemian from the model version with the most reduced Eemian ice sheet.
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