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 …

Over the past decades, significant efforts have been made to understand the nature,
dynamics and evolution of volcanic systems. In parallel, the continuous demographic …

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 …

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 …

This chapter reviews glacial isostatic adjustment (GIA) and post-seismic deformation in
Antarctica. It discusses numerical models and their inputs, and observations and inferences …

As seismic data collection continues to grow, advanced automated processing techniques
for robust phase identification and event detection are becoming increasingly important …

We investigate the occurrence of repeating glacial seismicity near the grounding line of the
Foundation Ice Stream and further upstream using continuous broadband seismic data …

Geothermal heat flow is a key parameter in governing ice dynamics, via its influence on
basal melt and sliding, englacial rheology, and erosion. It is expected to exhibit significant …

We apply a machine learning (ML) earthquake detection technique on over 21 yr of seismic
data from on‐continent temporary and long‐term networks to obtain the most complete …

We examine upper mantle anisotropy across the Antarctic continent using 102 new shear
wave splitting measurements obtained from teleseismic SKS, SKKS, and PKS phases …