In order to assess the range of plausible future LSL trajectories for the Dutch Coast, we will consider a number of scenarios for the forcing. S1 and S2 are basically extrapolations of the various factors into the future assuming a small uplift and a larger subsidence of the land, respectively. The contributions from ice sheets, glaciers, terrestrial hydrosphere and thermal expansion are taken from the AR4 of IPCC. For the other scenarios, except S7, we take S1 as a starting point. For S3 and S4, we assume an increased melting of Greenland and Antarctica, respectively. For S5, we increase the melting of glaciers and ice caps according to Meier et al. (2007). For S6 and S7, we assume both an increased melt of Antarctica and a larger contribution from glaciers and ice caps, with the starting scenarios being S1 and S2, respectively. S7 is certainly the most extreme scenario for the Dutch Coast.