Most of the WAIS is grounded below sea level and has the potential to collapse if grounding -
line retreat triggers a strong positive feedback whereby ocean water undercuts the ice sheet and triggers further separation from the bedrock (35 ⇓ — 37).
Not exact matches
A
retreat to that level, and a rebound, would
trigger an adjustment in the position of the up - sloping trend
line.
The height of these cliffs made them unstable,
triggering the release of thousands of icebergs into Pine Island Bay, and causing the glacier to
retreat rapidly until its grounding
line reached a restabilising point in shallower water.
For instance, if a particular sector has been shown to potentially experience ocean warming in the future — one of the main
triggers to grounding
line retreat — we would assign a relatively high probability; while a sector already experiencing grounding
line retreat would have a very high probability.