A key question has long been
whether ice sheet contribution could accelerate substantially, by an order of magnitude, either in this century or subsequently.
Not exact matches
Determining
whether polar
ice sheets are shrinking or growing, and what their
contribution to changes in sea level is, has motivated polar scientists for decades.
Consequently,
ice sheet contribution to sea level rise — even if it were the same amount — would have different impacts, depending on
whether the
contribution came from Greenland or Antarctica (Bamber and Riva 2010).