By the second half of this century, rising air
temperatures above the Weddell Sea could set off a self - amplifying meltwater feedback cycle
under the Filchner - Ronne
Ice Shelf, ultimately causing the second - largest ice shelf in the Antarctic to shrink dramatical
Ice Shelf, ultimately causing the second - largest
ice shelf in the Antarctic to shrink dramatical
ice shelf in the Antarctic to shrink dramatically.
Now, Bindschadler and other researchers are heading out to fetch some of the first
temperature data from
under the Pine Island Glacier
ice shelf, the outlet of one of the largest and fastest moving glaciers in Antarctica, in hopes of understanding what is happening beneath it.