Mass melting of the West Antarctic Ice Sheet was a major cause of high sea levels during a period known as the Last Interglacial (129,000-116,000 years ago), an international team of scientists led by UNSW's Chris Turney has found.
Mass melting of the West Antarctic Ice Sheet was a major cause of high sea levels during a period known as the Last Interglacial (129,000-116,000 years ago), an international team of scientists led by UNSW's Chris Turney has found. The research was published today in Proceedings of the National Academy of Sciences (PNAS). The extreme ice loss caused a multi-metre rise in global mean sea levels - and it took less than 2°C of ocean warming for it to occur.
"Not only did we lose a lot of the West Antarctic Ice Sheet, but this happened very early during the Last Interglacial," says Chris Turney, Professor in Earth and Climate Science at UNSW Sydney and lead author of the study.
Fine layers of ancient volcanic ash in the ice helped the team pinpoint when the mass melting took place. Alarmingly, the results indicated that most ice loss occurred within the first millennia, showing how sensitive the Antarctic is to higher temperatures.
Read more at University of New South Wales
Image by Siggy Nowak from Pixabay
