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 …

Geothermal heat flow (GHF) is an elusive physical property, yet it can reveal past and
present plate tectonic processes. In Antarctica, GHF has further consequences in predicting …

The marine portion of the West Antarctic Ice Sheet (WAIS) in the Amundsen Sea Embayment
(ASE) accounts for one-fourth of the cryospheric contribution to global sea-level rise and is …

We estimate the upper mantle temperature of the Antarctic Plate based on the thermoelastic
properties of mantle minerals and S velocities using a new 3‐D shear velocity model, AN1 …

The response of the Antarctic Ice Sheet (AIS) to climate change is the largest uncertainty in
projecting future sea level. The impact of three-dimensional (3D) Earth structure on the AIS …

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 upper mantle and transition zone beneath Antarctica and the surrounding oceans are
among the poorest‐imaged regions of the Earth's interior. Over the last 15 years, several …

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 …

A Coupled Ice Sheet–Sea Level Model Incorporating 3D Earth Structure: Variations in
Antarctica during the Last Deglacial Retreat in: Journal of Climate Volume 31 Issue 10 (2018) …