However, if
the remaining ice shelf collapses or starts losing mass more rapidly, it could effectively unplug the glaciers next to the shelf, sending land - based ice into Southern Ocean, and contributing to sea level rise.
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.
Only floating sea
ice (bottom right)
remains of the
collapsed Larsen B
ice shelf off the Antarctic Peninsula.
Losing a massive, state - sized
ice block may leave the
remaining shelf vulnerable to further climate change - related conditions and its
collapse will occur earlier, O'Leary explained.
By examining past
ice shelf collapse and projecting the next century of temperature change onto current
ice shelves, Trusel and his fellow researchers found a huge difference between a business - as - usual fossil fuel emission scenario, in which
ice melt may increase eight-fold, and a scenario where emissions are stabilized relatively rapidly and
ice melt
remains relatively linear.