The resulting projections for 2050, 2100, and 2200 illustrate the large range of plausible LSL changes in the future. For 2100, the total range of change is about 2 m, with a potential maximum rise of 1.25 m. For 2200, a much larger rise is possible. The main single process responsible for a large positive contribution would be an increased melting of parts of the Antarctic ice sheet. A large uncertainty comes from the Greenland ice sheet, both in terms of the melting itself but also in terms of the response of LSL at the Dutch coast to Greenland melting. With respect to the Greenland ice sheet, the Dutch coast is located in the region where the fingerprint changes from a negative to a positive response with relative large differences between different geophysical models. Some models predict a small positive contributions of Greenland melting to LSL at the Dutch coast, while other models predict a negative contribution.