Not exact matches
In contrast to
glaciers and ice sheets, which sit on the
ground,
ground ice sits in the
ground, mixed with frozen soil or buried
under layers of sediment.
Thwaites, meanwhile, also continues to rank among of the fastest - shrinking
glaciers, and has seen its
grounding line retreat rate increase slightly compared to the earlier period, which Konrad said «should emphasize once more that this
glacier is
under threat.»
Satellites have provided
grounding lines observations of Pine Island Thwaites
glaciers (and other
glaciers for that matter) since getting direct observations
under the ice is basically a non-starter.
And sea level rise will affect the
glaciers that have
grounding lines upstream and
under the ice — the
grounding line moves further upstream... would this touch some of the deeper lakes
under the ice cap?