A 40-y record reveals gradual Antarctic sea ice increases followed by decreases at rates far exceeding the rates seen in the Arctic
Geophysical constraints on the dynamics and retreat of the Barents Sea ice sheet as a paleobenchmark for models of marine ice sheet deglaciation
Sea Level Change Through the Last Glacial Cycle
Antarctic Sea Ice--a Habitat for Extremophiles
First observations of the interaction of ocean swell with sea ice using satellite radar altimeter data
