Stable grounding lines can not be established on these reverse bed slopes1, because ice thickness is a key factor in controlling ice flux across the grounding line.
Not exact matches
Now seafloor sediments reveal that Larsen B's
grounding line had remained
stable for thousands of years before the ice shelf's collapse.
If they begin to melt, however — particularly as they're exposed to warmer ocean water — the shelves become thinner and the
grounding line begins to retreat backward, causing the glacier to become less
stable and making the ice shelf more likely to break.
The MISI is based on a number of studies that indicated the theoretical existence of the instability... The most fundamental derivation, that is, starting from a first - principle ice equation, states that in one - dimensional ice flow the
grounding line between
grounded ice sheet and floating ice shelf can not be
stable on a landward sloping bed.
That means that either the water is finding a way to get up under the ice, or the
grounding line has moved inland from what had been a relatively
stable location from 1992 until 2011.
Most of the increase occurred along West Antarctic
grounding lines; East Antarctic glaciers remained very
stable.