"These results underscore the central role of ice sheets in future sea level rise", says Giorgio Spada, Professor at the Department of Physics and Astronomy - DIFA "Augusto Righi" of the University of Bologna, who took part in the study. "Their response to climate warming is the main source of uncertainty in projections, and a continuous half-century record of ice-sheet behaviour is therefore essential to predict the risks threatening the hundreds of millions of people living in low-lying coastal areas".
The historical series shows that ice losses have increased rapidly since the 1990s. Greenland, close to balance in the 1970s, saw its rate of loss rise from around 60 billion tonnes per year in the 1980s to 264 billion in the 2010s, a decade marked by repeated extreme summer melt events. Antarctica’s loss rate, meanwhile, rose from around 48 billion tonnes per year in the 1980s to 202 billion in the 2010s.
The most recent years (2020–2023) recorded a temporary slowdown in ice loss. Record snowfall over East Antarctica offset part of the glacial losses occurring elsewhere on the continent, while a series of milder summers in Greenland roughly halved surface melting. Scientists warn, however, that these are short-term oscillations against the backdrop of a clear long-term trend, not a reversal of ice loss.
The study was published in the journal Scientific Data under the title “Mass balance of the Greenland and Antarctic ice sheets from the 1970s to 2023”. For the University of Bologna, the study involved Giorgio Spada, a Professor at the Department of Physics and Astronomy - DIFA "Augusto Righi".