Even as Rignot and colleagues suggest that loss of the Amundsen Sea
embayment glaciers appears inevitable, it remains extremely difficult to predict exactly how this ice loss will unfold and how long it will take.
The pace and magnitude of the changes observed in this region match the expectation that Amundsen Sea
embayment glaciers should be less stable than others.
Not exact matches
In Antarctica, dynamic thinning has accelerated at the grounding lines of the major
glaciers of the Amundsen Sea
embayment, and in places has penetrated to within 100 km of the ice divides.
On the
glacier scale, thinning is strongest in the Amundsen Sea
embayment (ASE), where it is confirmed as being localized on the fast - flowing
glaciers and their tributaries (Fig. 3 [below].
There was a paper in Science several years back whose conclusion was that once
glaciers left their terminal moraine grounding lines behind, the
embayment left behind would freshen and cool with meltwater and provide a negative feedback to more melting.