Comparing the Simulated Surface Mass Balance of the Laurentide Ice Sheet During the Last Deglaciation With a Geophysical Reconstruction
Despite decades of research, our understanding of the role of climate feedbacks in shaping Pleistocene glacial cycles remains incomplete. Here, we investigate the decay of the Laurentide Ice Sheet (LIS) by calculating its surface mass balance (SMB) during the last deglaciation using the isotope‐enabled transient clim...