Mass loss from the Antarctic Ice Sheet is dominated by ice dynamics, where ocean-driven
melt leads to un-buttressing and ice flow acceleration. Long-term ice speed change has …

Relatively little is known about the physical mechanisms that drive the dynamics of the East
Antarctic outlet glaciers. Here we conduct a remote-sensing investigation of the Polar …

Recent satellite-remote sensing studies have documented the multi-decadal acceleration of
the Antarctic Ice Sheet in response to rapid rates of ice-sheet retreat and thinning. Unlike the …

Ice discharge from large ice sheets plays a direct role in determining rates of sea-level rise.
We map present-day Antarctic-wide surface velocities using Landsat 7 and 8 imagery …

Atmospheric warming is increasing surface melting across the Antarctic Peninsula, with
unknown impacts upon glacier dynamics at the ice-bed interface. Using high-resolution …

We constructed Antarctic ice velocity maps from Landsat 8 images for the years 2014 and
2015 at a high spatial resolution (100 m). These maps were assembled from 10,690 scenes …

Antarctica's contribution to global mean sea level rise has been driven by an increase in ice
discharge into the oceans. The rate of change and the mechanisms that drive variability in …

Totten Glacier has the largest ice discharge in East Antarctica and a basin grounded mostly
below sea level. Satellite altimetry data have revealed ice thinning in areas of fast flow. Here …

West Antarctica has experienced dramatic ice losses contributing to global sea-level rise in
recent decades, particularly from Pine Island and Thwaites glaciers. Although these ice …

Ice dynamic change is the primary cause of mass loss from the Antarctic Ice Sheet, thus it is
important to understand the processes driving ice-ocean interactions and the timescale on …