Figure 11.13: Sea level
change in metres over the 21st century resulting from thermal expansion and ocean
circulation changes calculated from AOGCM experiments following the IS92a scenario
and including the direct effect of sulphate aerosol (except that ECHAM4/OPYC3
G is shown instead of GS, because GS ends in 2050). Each field is the difference
in sea level change between the last decade of the experiment and the decade 100
years earlier. See Tables 8.1 and 9.1 for further details of models and experiments.