Coming just a few days after research showing West Antarctic glaciers are in irreversible collapse, Monday's news that Antarctic ice melt has doubled in a decade was widely covered.
We've taken a look at several new papers that highlight the speed at which earth's vast ice sheets, glaciers, and ice caps are diminishing. Put them all together, and it makes for a stark picture.
- Antarctic ice melt is twice as fast as ten years ago
'Antarctic ice losses have doubled in less than a decade with 159 billion tonnes of ice melting each year', reads Monday's Daily Mail headline. The Guardian opts for, 'Doubling of Antarctic ice loss revealed by European satellite'. The Times says 'Antarctic melt rate worries scientists'.
All three headlines stem from a paper published yesterday in Geophysical Research Letters, which finds the volume of ice melting into the ocean from Antarctica is twice as large the average between 1992 and 2011, now raising global sea levels by 0.45 millimetres a year.
Across Antarctica, the average height of the ice is dropping by 1.9 centimetres per year, the data show. East Antarctica is staying roughly the same, but West Antarctica is seeing big losses, where ice melt is 31 per cent faster now than between 2005 and 2011. Ice loss from glaciers along the Amundsen coast has tripled over the past two decades. - West Antarctic glaciers are collapsing, and it's "unstoppable"
Not only are the glaciers shrinking, but there's nothing to stop them melting completely. That's why scientists are talking about the glaciers' collapse as "irreversible" and "unstoppable". And without the huge glaciers to prop up the interior of the ice sheet, much larger areas of West Antarctic ice will start slipping into the ocean. This would ultimately raise sea levels by three to four metres, though that would take several centuries, say the scientists. - The Greenland ice sheet could melt faster than scientists first thought
The Greenland ice sheet may be more vulnerable to climate change than previously thought, scientists reported in a Nature Geoscience paper on Sunday. The team of US scientists discovered deep channels extending horizontally below the surface of the Greenland sheet, which mean large parts of the glaciers lie on land that's below sea level. Just like in West Antarctic glaciers, warm water coming into contact with the edge of the glacier forms vast pools under the ice sheet, melting it from the bottom up, the paper explains. - Other ice caps and glaciers in the northern hemisphere are melting faster too
As well as the Greenland and Antarctic ice sheets, glaciers and ice caps on land are also melting under the pressure of rising temperatures and contributing to sea level rise. A new paper published Monday in the Journal of Climate looks at ice-covered areas greater or equal to 0.5 square kilometres in the Northern Hemisphere, excluding the Greenland Ice Sheet. The researchers built a model of glacier and ice cap responses to past temperature and snowfall changes, testing it against nearly 1500 measurements from 78 locations worldwide. The scientists estimated the total contribution to sea-level rise from ice caps and glaciers was 0.51 millimetres per year between 1979-2009. But it's speeding up - looking just at the recent decade, 1999-2009, the contribution is 40 per cent higher, at around 0.71 millimetres per year. - Soot from forest fires contributed to unusually large Greenland surface melt in 2012
Finally, a new study published Monday explores the reasons for why an unusually large amount of the surface of the Greenland ice sheet melted in 2012. This exceptional summer saw more than 97 percent melt away, far more than the next biggest event almost a century before in 1889. The team of US scientists examined the layers of ice and snow in six ice cores, concluding that a combination of exceptionally high temperatures and soot from northern hemisphere forest fires, known as black carbon, drove unusually extensive surface melt in both cases.
Surface melting doesn't contribute to sea level rise because the water percolates back into the snow and refreezes. But it does reduce the reflectivity of the ice, known as albedo, with consequences for how much sunlight the Arctic region absorbs, and how much ice stays frozen.
Together, with soot which also decreases reflectivity, the ice albedo was pushed below a certain threshold in 1889 and 2012, making it vulnerable to rapid ice loss, say the authors. Lead author Kaitlin Keegan explains such big surface melting events won't be out of place by 2100: "With both the frequency of forest fires and warmer temperatures predicted to increase with climate change, widespread melt events are likely to happen much more frequently in the future."
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