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 …

We construct a new seismic model for central and West Antarctica by jointly inverting
Rayleigh wave phase and group velocities along with P wave receiver functions. Ambient …

The seismic velocity structure of Antarctica is important, both as a constraint on the tectonic
history of the continent and for understanding solid Earth interactions with the ice sheet. We …

The possibility that a deep mantle plume manifests Pliocene and Quaternary volcanism and
potential elevated heat flux in West Antarctica has been studied for more than 30 years …

The dynamics of the ice sheets on glacial timescales are highly controlled by interactions
with the solid Earth, ie, the glacial isostatic adjustment (GIA). Particularly at marine ice …

Seismographic coverage of Antarctica prior to 2007 consisted overwhelmingly of a handful
of long running and sporadically deployed transient stations, many of which were principally …

We employ a coupled model for ice-sheet dynamics and Maxwell viscoelastic solid-Earth
dynamics, including a gravitationally consistent description of sea level. With this model, we …

The effect of finite strain geometry on crystallographic preferred orientation (CPO) is poorly
constrained in the upper mantle. Specifically, the relationship between shape preferred …

The deployment of seismic stations and the development of ambient noise tomography as
well as new analysis methods provide an opportunity for higher-resolution imaging of …

The vast majority of ice-sheet modelling studies rely on simplified representations of the
glacial isostatic adjustment (GIA), which, among other limitations, do not account for lateral …