The ice shelves in the Bellingshausen Sea are melting and thinning rapidly due to modified
Circumpolar Deep Water (mCDW) intrusions carrying heat toward ice‐shelf cavities …

Abstract The northern Antarctic Peninsula (NAP) is a highly dynamic transitional zone
between the subpolar-polar and oceanic-coastal environments, and it is located in an area …

Processes driving changes in sea-ice seasonality and sea-ice thickness were explored for a
'warm-shelf'region along the West Antarctic Peninsula using vertically coupled sea-ice …

The vertical front of ice shelves represents a topographic barrier for barotropic currents that
transport a considerable amount of heat toward the ice shelves. The blocking effect of the ice …

Abstract Barotropic (ie, depth-uniform) coastal oceanic Kelvin waves can provide rapid
teleconnections from climate and weather events in one location to remote regions of the …

We analyze several year‐long moored current meter records collected on the midshelf and
shelf break of the western Antarctic Peninsula in order to describe the major features of the …

Antarctic ice shelves are the link between the Southern Ocean and the Antarctic Ice Sheet.
The floating ice shelves restrain the seaward flow of the grounded ice, which is balanced by …