Melting of Northern Greenland during the last interglaciation A. Born

Assuming that the climate obtained from REMBO is fairly well represented but other processes (such as fast flow in the ice sheet model) are ignored, we believe that there are then

pachyderma (sin) for the Marine Isotope Stages 6 to present. 2) Investigate how the offshore record aligns with the variability of the Greenland Ice Sheet in the last glacial,

Ocean thermal forcing used in Coupled Model Intercomparison Project phase 6 (CMIP6)-forced experiments for Antarctic ice sheet (AIS) sectors (a) Pine Island and Thwaites glaciers,