\t\t\t\t\t\t28\/11\/2023<\/span> With all eyes about to focus on the COP28 climate conference in Dubai, new scientific findings show, again, that the climate crisis is taking its toll on Antarctica \u2013 a continent, up to recently, thought better able to withstand the immediate effects of rising global temperatures.<\/p>\n Using satellite data, scientists have discovered that the ice shelf extending into the ocean from Cadman Glacier on the west Antarctic Peninsula collapsed, leaving the glacier exposed to unusually warm ocean water, which caused the glacier to accelerate and retreat rapidly.<\/p>\n<\/div>\n The research, published today in Nature Communications<\/i>, describes how a team of scientists from the University of Leeds, Lancaster University, ENVEO, the University of Delaware and the British Antarctic Survey, used data from nine different satellite missions, including ESA\u2019s CryoSat and Europe\u2019s Copernicus Sentinel-1, along with in-situ measurements to map how the floating ice shelf and glacier changed.<\/p>\n They found that between November 2018 and May 2021, the glacier retreated a whopping eight kilometres, after being stable for around 50 years.<\/p>\n They conclude that unusually high ocean water temperatures around the west Antarctic Peninsula in 2018\u20132019 have triggered the Cadman Glacier system to change dramatically.<\/p>\n<\/p><\/div>\n \t\t\t\t<\/p>\n <\/figcaption><\/figure>\n Benjamin Wallis, from the University of Leeds who led the research, explained, \u201cBy tracking Cadman Glacier with satellites we saw that it started speeding up massively in 2018, and when we investigated ocean reanalysis data, we found that the waters nearby were up to 2\u00b0C warmer than average at that time.<\/p>\n \u201cWe think the warmer waters gradually started to eat away at the Cadman Ice Shelf from the early 2000s, but possibly from as early as the 1970s.<\/p>\n \u201cThe warmer water was not only on the surface of the ocean, but also deep in the water column. This warmer water may have reached to where the shelf was grounded on the sea floor. The result being that the ice shelf was melting from the bottom up, which we were able to observe using satellite data.\u201d<\/p>\n Extending from glaciers on land, ice shelves float on the ocean surface and sometime reach the ocean floor where then can be anchored, or grounded.<\/p>\n Importantly, ice shelves act as a buttress, slowing the flow of the glacier towards the sea.<\/p>\n<\/p><\/div>\n The Cadman Ice Shelf became so thin that it was no longer able to hold back the glacier.<\/p>\n In 2019, the shelf broke free from the grounding zone, in effect slipping anchor and enabling the Cadman Glacier to speed up and drain more ice into the sea.<\/p>\n According to this new research, the Cadman Glacier is now in a state of \u2018substantial dynamic imbalance\u2019.<\/p>\n The ice on the glacier has continued to thin, losing 20 metres a year in height, which is equivalent to a loss in height of a five-storey building each year.\u00a0<\/p>\n And around 2.16 billion tonnes of ice are draining from the Cadman Glacier into the ocean each year.<\/p>\n<\/p><\/div>\n \u201cCuriously, neighbouring glaciers on this part of the west Antarctic Peninsula did not react in the same way, which may hold important lessons for the way we can better project how climate change will continue to affect this important and sensitive polar region,\u201d noted Benjamin Wallis.<\/p>\n The researchers say what has happened to the Cadman Glacier can be seen as an example of a \u2018glaciological tipping point\u2019, where a system in a steady state can take one or two paths based on a change in an environmental parameter.\u00a0<\/p>\n A tipping point was reached in 2018 caused by the arrival of unusually warm ocean water, which caused the ice shelf to unground. Reaching this tipping point caused Cadman Glacier to increase its ice discharge by 28% in 13 months.\u00a0<\/p>\n Prof. Michael Meredith, from the British Antarctic Survey and one of the authors of the paper, said, \u201cWe have known for some time that the ocean around Antarctica is heating up rapidly, and that this poses a significant threat to glaciers and the ice sheet, with consequences for sea-level rise globally.<\/p>\n \u201cWhat this new research shows is that apparently stable glaciers can switch very rapidly, becoming unstable almost without warning, and then thinning and retreating very strongly.<\/p>\n<\/p><\/div>\n \u201cThis emphasises the need for a comprehensive ocean observing network around Antarctica, especially in regions close to glaciers that are especially hard to make measurements.\u201d\u00a0<\/p>\n ESA\u2019s Mark Drinkwater added, \u201cAgain we see that the Antarctic is more susceptible to change than we thought a few years ago. It is imperative that we continue to monitor this fragile continent and surrounding oceans. We can only capture the full extent of such changes with pan-Antarctic measurements obtained by satellites over decades.<\/p>\n \u201cThankfully, we have missions such as CryoSat and Copernicus Sentinel-1 in orbit, but, importantly, we are developing new satellite missions such as the Copernicus Sentinel Expansion Mission Cristal and Sentinel-1 Next Generation to continue, to sustain, and enhance these types of measurements in the future.\u201d<\/p>\n<\/p><\/div>\n
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