Some ocean modeling studies have identified a potential tipping point from a low to a high
basal melt regime beneath the Filchner–Ronne Ice Shelf (FRIS), Antarctica, with significant …

The Antarctic Peninsula has seen rapid and widespread changes in the extent of its ice
shelves in recent decades, including the collapse of the Larsen A and B ice shelves in 1995 …

Mass loss from ice shelves is a strong control on grounding-line dynamics. Here we
investigate how calving and submarine melt parameterizations affect steady-state grounding …

Many floating ice shelves in Antarctica buttress the ice streams feeding them, thereby
reducing the discharge of icebergs into the ocean. The rate at which ice shelves calve …

Basal ice-shelf melting is the key driver of Antarctica's increasing sea-level contribution. In
diminishing the buttressing force of the ice shelves that fringe the ice sheet, the melting …

Antarctica's Lambert Glacier drains about one-sixth of the ice from the East Antarctic Ice
Sheet and is considered stable due to the strong buttressing provided by the Amery Ice …

When subglacial meltwater is discharged into the ocean at the grounding line, it acts as a
source of buoyancy, enhancing flow speeds along the ice base that result in higher basal …

The timescales of the flow and retreat of Greenland's and Antarctica's outlet glaciers and
their potential instabilities are arguably the largest uncertainty in future sea-level projections …

Some ocean modeling studies have identified a potential tipping point from a low to high
basal melt regime beneath the Filchner-Ronne Ice Shelf (FRIS), Antarctica, with significant …

Antarctica's Lambert Glacier drains about one-sixth of the ice from the East Antarctica Ice
Sheet and is considered stable due to the strong buttressing provided by the Amery Ice …