Global warming has caused extreme ice melting events in Greenland to become more frequent and more intense over the past 40 years according to new research, raising sea levels and flood risk worldwide.

Over the past decade alone, 3.5 trillion tonnes of ice has melted from the surface of the island and flowed downhill into the ocean.

That’s enough melted ice to cover the entire UK with around 15 metres of meltwater, or cover the entire city of New York with around 4500 metres.

The new study, including Lancaster University’s Dr Amber Leeson and led by the University of Leeds, is the first to use satellite data to detect this phenomena – known as ice sheet runoff – from space.

The findings, published in Nature Communications, reveal that Greenland’s meltwater runoff has risen by 21% over the past four decades and has become 60% more erratic from one summer to the next.

Lead author Dr Thomas Slater, a Research Fellow in the Centre for Polar Observation and Modelling at the University of Leeds said:

“As we’ve seen with other parts of the world, Greenland is also vulnerable to an increase in extreme weather events.

“As our climate warms, it’s reasonable to expect that the instances of extreme melting in Greenland will happen more often – observations such as these are an important step in helping us to improve climate models and better predict what will happen this century.”

The study, funded by the European Space Agency’s (ESA) as part of its Polar+ Surface Mass Balance Feasibility project, used measurements from the ESA’s CryoSat-2 satellite mission.

The research shows that over the past decade (2011 to 2020), increased meltwater runoff from Greenland raised the global sea level by one centimetre. One third of this total was produced in just two hot summers (2012 and 2019), when extreme weather led to record-breaking levels of ice melting not seen in the past 40 years.

Raised sea levels caused by ice melt heightens the risk of flooding for coastal communities worldwide and disrupts marine ecosystems in the Arctic Ocean that indigenous communities rely on for food.

It can also alter patterns of ocean and atmospheric circulation which affect weather conditions around the planet.

During the past decade, runoff from Greenland has averaged 357 billion tonnes per year, reaching a maximum of 527 billion tonnes of ice melt in 2012, when changes in atmospheric patterns caused unusually warm air to sit over much the ice sheet. This was more than twice the minimum runoff of 247 billion tonnes that occurred in 2017.

The changes are related to extreme weather events, such as heatwaves, which have become more frequent and are now a major cause of ice loss from Greenland because of the runoff they produce.

Dr Slater said: “There are, however, reasons to be optimistic. We know that setting and meeting meaningful targets to cut emissions could reduce ice losses from Greenland by a factor of three, and there is still time to achieve this.”

These first observations of Greenland runoff from space can also be used to verify how climate models simulate ice sheet melting which, in turn, will allow improved predictions of how much Greenland will raise the global sea level in future as extreme weather events become more common.

Study co-author Dr Amber Leeson, Senior Lecturer in Environmental Data Science at Lancaster University, said:

“Model estimates suggest that the Greenland ice sheet will contribute between about 3 and 23 cm to global sea level rise by 2100.

“This prediction has a wide range, in part because of uncertainties associated with simulating complex ice melt processes, including those associated with extreme weather. These new spaceborne estimates of runoff will help us to understand these complex ice melt processes better, improve our ability to model them, and thus enable us to refine our estimates of future sea level rise.”

Finally, the study shows that satellites are able to provide instant estimates of summer ice melting, which supports efforts to expand Greenland’s hydropower capacity and Europe’s ambition to launch the CRISTAL mission to succeed CryoSat-2.

ESA’s CryoSat mission manager, Tommaso Parrinello, said:

“Since it was launched over 11 years ago, CryoSat has yielded a wealth of information about our rapidly changing polar regions. This remarkable satellite remains key to scientific research and the indisputable facts, such as these findings on meltwater runoff, that are so critical to decision-making on the health of our planet.

“Looking further to the future, the Copernicus Sentinel Expansion mission CRISTAL will ensure that Earth’s vulnerable ice will be monitored in the coming decades. In the

meantime, it is imperative that CryoSat remains in orbit for as long as possible to reduce the gap before these new Copernicus missions are operational.”

“Increased variability in Greenland Ice Sheet runoff from satellite observations” is published 1 November in Nature Communications.

https://dx.doi.org/10.1038/s41467-021-26229-4