Another interesting paper is Meier et al., Science, 317, 2007, wherein they point out that glaciers (as opposed to Greenland Ice sheet and Antarctica) have dominated
the eustatic contribution in this century.
Not exact matches
We obtain a value for the global,
eustatic sea - level rise
contribution of about 3.3 meters, with important regional variations.
We reassess the potential
contribution to
eustatic and regional sea level from a rapid collapse of the ice sheet and find that previous assessments have substantially overestimated its likely primary
contribution.
Antarctica's
contribution to
eustatic sea level during meltwater pulse - 1A.
Satellite measurements of the Patagonian icefields suggest that they are currently rapidly receding and thinning, with a measureable
contribution to
eustatic sea level rise2.
Our approach estimates the
eustatic sea - level
contribution to the palaeobathymetry curve by placing constraints on total subsidence and decompacted sediment accumulation.