A new scientific study could prove helpful in accurately predicting rising levels 

UK-based research discusses the demand to monitor short – and long – term timescales of changes in ice sheet behaviour to reduce uncertainty in future sea level rise projections

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As one of the most pressing issues of the current time, climate change has caused significant rises in sea levels. Trying to accurately predict just how much they will rise in the future is subject to ongoing analysis. A crucial factor in the projection of future sea level rise is the acknowledgement of the changing nature of the ice sheets.

It was previously thought that ice sheets, the gigantic stores of ice in Antarctica and Greenland that lock up sea water, equivalent to an increase of 65 metres in global sea level rise, were relatively static, slow-moving, and slow to respond to climate change. However, the research illustrated that these huge glaciers respond far quicker and unexpectedly as the climate warms, in a similar way that the frequency and intensity of hurricanes and heatwaves change with the climate.

Ground and satellite observations and the development of climate models demonstrate that sudden heatwaves and large storms can have long-lasting effects on the ice sheets. This weather fluctuation can lead to extreme melt events, such as the Greenland ice sheet melt in July 2023, or cause ice shelves to disappear almost overnight, as with the Antarctica Conger Ice Shelf collapse in 2022.

Published in the journal Nature Reviews Earth & Environment, the research discusses the demand to monitor short- and long-term timescales of changes in ice sheet behaviour to reduce uncertainty in future sea level rise projections.

The study highlights that predictions of sea level rise could be refined to better prepare for the effects of climate change. Glacial masses are subject to short-term fluctuations and extreme events across a wide range of timescales, from days to thousands of years, and as a result, diverse knowledge should be gathered.

Under the direction of Edward Hanna, Professor of Climate Science and Meteorology at the University of Lincoln, an international group of interdisciplinary scientists reviewed the evidence gathered from observational data, geological records, and computer model simulations.

A prominent aspect of the review indicated that short-term fluctuations in climate could have an amplification feedback effect, meaning that ice sheets are more sensitive to climate change than previously understood.

Edward Hanna, Professor of Climate Science and Meteorology at the University of Lincoln, said: “How the giant ice sheets of Antarctica and Greenland respond to ongoing climate change is crucial for determining the rate of sea-level rise over the next few decades and centuries. Ice sheet mass loss is not a simple, uniform response to climate warming. However, it is punctuated, for example, by short-term, typically several days-long extreme melting events and by the catastrophic break-up of ice shelves along the coast, which can occur rapidly, unplugging much larger amounts of ice from further inland.”

She also shared that the patterns, processes, and effects of ice sheet variability on different timescales, from days through millennia, are not well understood. Failing to account for such variability can, in turn, result in biassed projections of multi-decadal future ice sheet mass loss. The time to act is now, and improving projections through collaborative efforts will help us pave the way for a more sustainable future.

This review serves as a call to action, urging the scientific community to prioritise research efforts that will enhance the understanding of ice sheet variability. It is crucial that scientists, policymakers, and stakeholders collaborate more closely to improve climate and ocean monitoring systems, refine models, and ensure that ice sheet models accurately represent the observed changes, the research suggests.

The research was sponsored by the World Climate Research Programme’s Climate and Cryosphere project, the International Arctic Science Committee, and the Scientific Committee on Antarctic Research and resulted from a collaboration following an Ice Sheet Mass Balance and Sea Level expert group workshop.