Ice losses from Antarctica have increased global sea levels by 7.6 mm since 1992, with two fifths of this rise (3 mm) coming in the last five years alone.
The findings are from a major climate assessment known as the Ice Sheet Mass Balance Inter-comparison Exercise (IMBIE), and are published today in Nature.
It is the most complete picture of Antarctic ice sheet change to date 84 scientists from 44 international organisations combined 24 satellite surveys to produce the assessment.
We have long suspected that changes in Earths climate will affect the polar ice sheets. Thanks to the satellites, we can now track their ice losses and global sea level contribution with confidence.
The assessment, led by Professor Andrew Shepherd at the University of Leeds and Dr Erik Ivins at NASAs Jet Propulsion Laboratory in California, was supported by the European Space Agency (ESA) and the US National Aeronautics and Space Administration (NASA).
Their findings show that prior to 2012, Antarctica lost ice at a steady rate of 76 billion tonnes per year a 0.2 mm per year contribution to sea level rise. However, since then there has been a sharp, threefold increase. Between 2012 and 2017 the continent lost 219 billion tonnes of ice per year a 0.6 mm per year sea level contribution.
Antarctica stores enough frozen water to raise global sea level by 58 metres, and knowing how much ice it is losing is key to understanding the impacts of climate change today and in the future.
Professor Shepherd said: We have long suspected that changes in Earths climate will affect the polar ice sheets. Thanks to the satellites our space agencies have launched, we can now track their ice losses and global sea level contribution with confidence.
According to our analysis, there has been a steep increase in ice losses from Antarctica during the past decade, and the continent is causing sea levels to rise faster today than at any time in the past 25 years. This has to be a concern for the governments we trust to protect our coastal cities and communities.
Dr Ivins said: The added duration of the observing period, the larger pool of participants, various refinements in our observing capability and an improved ability to assess both inherent and interpretive uncertainties, each contribute to making this the most robust study of ice mass balance of Antarctica to date.
University of Leeds scientists ice coring at the George VI Ice Shelf, Antarctica. Picture: Ian Potten, British Antarctic Survey
The threefold increase in ice loss from the continent as a whole is a combination of glacier speedup in West Antarctica and at the Antarctic Peninsula, and reduced growth of the ice sheet in East Antarctica.
West Antarctica experienced the largest change, with ice losses rising from 53 billion tonnes per year in the 1990s to 159 billion tonnes per year since 2012. Most of this came from the huge Pine Island and Thwaites Glaciers, which are retreating rapidly due to ocean melting.
At the northern tip of the continent, ice shelf collapse at the Antarctic Peninsula has driven a 25 billion tonne per year increase in ice loss since the early 2000s.
The East Antarctic ice sheet has remained close to a state of balance over the past 25 years, gaining just 5 billion tonnes of ice per year on average.
The paper Mass balance of the Antarctic ice sheet from 1992 to 2017 by the IMBIE Team, is published in Nature on 14 June. DOI: 10.1038/s41586-018-0179-y.
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Main image: Unusual iceberg at Rothera Research Station, Antarctic Peninsula, by Professor Andrew Shepherd