Solid Earth change and the evolution of the Antarctic ice sheet
Recent studies suggest that Antarctica has the potential to contribute up to ~15 m of sea-level rise over the next few centuries.
The evolution of the Antarctic Ice Sheet is driven by a combination of climate forcing and non-climatic feedbacks. In this review we focus on feedbacks between the Antarctic Ice Sheet and the solid Earth, and the role of these feedbacks in shaping the response of the ice sheet to past and future climate changes.