Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …

Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …

Accurate models of past Antarctic ice sheet behaviour require realistic reconstructions of the
evolution of bedrock topography. However, other than a preliminary attempt to reconstruct …

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 …

Cenozoic evolution of the Antarctic ice sheets is thought to be driven primarily by long-term
changes in radiative forcing, but the tectonic evolution of Antarctica may also have played a …

Abstract Early to Middle Miocene sea-level oscillations of approximately 40–60 m estimated
from far-field records,–are interpreted to reflect the loss of virtually all East Antarctic ice …

The view from the south is, more than ever, dominated by ominous signs of change.
Antarctica and the Southern Ocean are intrinsic to the Earth system, and their evolution is …

We implement a Coulomb rate‐and‐state approach to explore the nonlinear relation
between stressing rate and seismicity rate in the Groningen gas field. Coulomb stress rates …

Abstract The Southern Ocean is a key player in the climate, ocean, and atmospheric system.
As the only direct connection between all three major oceans since the opening of the …

Ice sheet behavior is strongly influenced by the bed topography. However, the effect of the
progressive temporal evolution of Antarctica's subglacial landscape on the sensitivity of the …