...One key interval of particular interest during the Pliocene is the mid-Piacenzian Warm Period – some 3.264 to 3.025 million years ago - when temperatures were 2 to 3º Celsius higher than pre-industrial levels. “The interval also marks the last time the Earth’s atmospheric CO2 was as high as today, providing important clues about what the future holds in the face of current anthropogenic warming,” Onac says.
This study found that during this period, global mean sea level was as high as 16.2 meters (with an uncertainty range of 5.6 to 19.2 meters) above present. This means that even if atmospheric CO2 stabilizes around current levels, the global mean sea level would still likely rise at least that high, if not higher, the scientists concluded. In fact, it is likely to rise higher because of the increase in the volume of the oceans due to rising temperature.
“Considering the present-day melt patterns, this extent of sea-level rise would most likely be caused by a collapse of both Greenland and the West Antarctic ice sheets,” Dumitru said.
The authors also measured sea level at 23.5 meters higher than present about four million years ago during the Pliocene Climatic Optimum, when global mean temperatures were up to 4°C higher than pre-industrial levels. “This is a possible scenario if active and aggressive reduction in green house gases into the atmosphere is not undertaken,” Asmerom said.