Antarctic landfast sea ice (fast ice) is stationary sea ice that is attached to the coast,
grounded icebergs, ice shelves, or other protrusions on the continental shelf. Fast ice forms …

A growing number of satellites in the outer solar system likely have global oceans beneath
their outer icy shells. While the presence of liquid water makes these ocean worlds …

Basal melt of ice shelves is not only an important part of Antarctica's ice sheet mass budget,
but it is also the origin of platelet ice, one of the most distinctive types of sea ice. In many …

Frazil ice comprises millimeter-sized ice crystal particles or flocculations in water, and its
generation and evolution primarily occur during the initial stage of the river ice process …

Antarctic sea ice that has been affected by supercooled Ice Shelf Water (ISW) has a unique
crystallographic structure and is called platelet ice. In this paper we synthesize platelet ice …

We investigate the structure and evolution of multiphase ice-ocean interfaces ('mushy
layers') and the implications for the geophysics and habitability of ice-ocean worlds …

In this paper we report measurements from the first year‐round mooring underneath sea ice
in McMurdo Sound, Antarctica, which we combine with full‐depth ocean profiles to identify …

We use new observations in Western McMurdo Sound, combined with longitudinal
hydrographic transects of the sound, to identify a northward‐flowing Ice Shelf Water (ISW) …

Variability in the volume of supercooled Ice Shelf Water outflow in McMurdo Sound is
reflected in the thickness and distribution of fast ice and the sub‐ice platelet layer beneath …

The formation of platelet ice is well known to occur under Antarctic sea ice, where subice
platelet layers form from supercooled ice shelf water. In the Arctic, however, platelet ice …