An attempt to quantify eustatic sea level fluctuations — A geological perspective

The complete meltdown of the Greenland and Antarctic ice sheets would raise the sea level 65 meters, whereas a partial meltdown only a few tens of meters. Eustatic sea level rates of changes in Greenland since 2003 show a net ice mass reduction of 96 gigatons per year; with this, geologists are called upon to add a historical perspective upon these changes.