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Bolstering concerns that so-called "feedback loops" should be considered a legitimate and serious concern, a new study shows that a worrying hypothesis put out just three years ago about the impacts of melting Antarctic ice may already have started coming true.
In a paper published in Science Advances, researchers at the University of Tasmania and other institutions found that the melting of Antarctica's glaciers has begun to trigger a "feedback loop" in which that melting's effects on the oceans cause even more ice sheets to deteriorate, and so on.
Chris Mooney of the Washington Post described the feedback loop phenomenon as "one of the most worrisome predictions about climate change" in an article about the findings.
"What we found is not only a modeling study but is something that we observed in the real ocean," Alessandro Silvano, one of the researchers, told the Post. "Our study shows for the first time actual evidence of this mechanism. Our study shows that it is already happening."
As Common Dreams reported in 2015, NASA climate scientist James Hansen first raised concerns about the feedback loop then. As the Post reports, Hansen explained that the melting of glaciers would create fresh water, blocking cold salt water from sinking to the bottom of the ocean and protecting the ice shelves from melting:
When cold surface water no longer sinks into the depths, a deeper layer of warm ocean water can travel across the continental shelf and reach the bases of glaciers, retaining its heat as the cold waters remain above. This warmer water then rapidly melts the glaciers and the large floating ice shelves connected to them.
The continuous melting cycle could soon begin to cause rapidly-rising sea levels and destructive hurricanes and other storms.
"That would mean loss of all coastal cities, most of the world's large cities and all their history," said Hansen when his paper on the feedback loop theory was released.
Hansen told the Post that the new research "provides a nice small-scale example" of the patterns he predicted.
"If we stay on business-as-usual [greenhouse gas] emissions rates, so that global warming continues to increase, I expect that the freshwater injection rate will increase (mainly via ice faster ice shelf breakup and underwater melt) and sea ice area will increase. This experiment will be playing out over the next years and decades," said Hansen in an email to the Post.
Anders Levermann, a climate scientist at the Potsdam Institute for Climate Impact Research, noted that it was "curious" that the feedback loop "is occurring now, after 10,000 years of stability, while we are ramping up the temperature of the planet."
"Trying to dismiss the idea that it has anything to do with global warming is also very difficult," he told the Scientific American.
Dear Common Dreams reader, It’s been nearly 30 years since I co-founded Common Dreams with my late wife, Lina Newhouser. We had the radical notion that journalism should serve the public good, not corporate profits. It was clear to us from the outset what it would take to build such a project. No paid advertisements. No corporate sponsors. No millionaire publisher telling us what to think or do. Many people said we wouldn't last a year, but we proved those doubters wrong. Together with a tremendous team of journalists and dedicated staff, we built an independent media outlet free from the constraints of profits and corporate control. Our mission has always been simple: To inform. To inspire. To ignite change for the common good. Building Common Dreams was not easy. Our survival was never guaranteed. When you take on the most powerful forces—Wall Street greed, fossil fuel industry destruction, Big Tech lobbyists, and uber-rich oligarchs who have spent billions upon billions rigging the economy and democracy in their favor—the only bulwark you have is supporters who believe in your work. But here’s the urgent message from me today. It's never been this bad out there. And it's never been this hard to keep us going. At the very moment Common Dreams is most needed, the threats we face are intensifying. We need your support now more than ever. We don't accept corporate advertising and never will. We don't have a paywall because we don't think people should be blocked from critical news based on their ability to pay. Everything we do is funded by the donations of readers like you. When everyone does the little they can afford, we are strong. But if that support retreats or dries up, so do we. Will you donate now to make sure Common Dreams not only survives but thrives? —Craig Brown, Co-founder |

Bolstering concerns that so-called "feedback loops" should be considered a legitimate and serious concern, a new study shows that a worrying hypothesis put out just three years ago about the impacts of melting Antarctic ice may already have started coming true.
In a paper published in Science Advances, researchers at the University of Tasmania and other institutions found that the melting of Antarctica's glaciers has begun to trigger a "feedback loop" in which that melting's effects on the oceans cause even more ice sheets to deteriorate, and so on.
Chris Mooney of the Washington Post described the feedback loop phenomenon as "one of the most worrisome predictions about climate change" in an article about the findings.
"What we found is not only a modeling study but is something that we observed in the real ocean," Alessandro Silvano, one of the researchers, told the Post. "Our study shows for the first time actual evidence of this mechanism. Our study shows that it is already happening."
As Common Dreams reported in 2015, NASA climate scientist James Hansen first raised concerns about the feedback loop then. As the Post reports, Hansen explained that the melting of glaciers would create fresh water, blocking cold salt water from sinking to the bottom of the ocean and protecting the ice shelves from melting:
When cold surface water no longer sinks into the depths, a deeper layer of warm ocean water can travel across the continental shelf and reach the bases of glaciers, retaining its heat as the cold waters remain above. This warmer water then rapidly melts the glaciers and the large floating ice shelves connected to them.
The continuous melting cycle could soon begin to cause rapidly-rising sea levels and destructive hurricanes and other storms.
"That would mean loss of all coastal cities, most of the world's large cities and all their history," said Hansen when his paper on the feedback loop theory was released.
Hansen told the Post that the new research "provides a nice small-scale example" of the patterns he predicted.
"If we stay on business-as-usual [greenhouse gas] emissions rates, so that global warming continues to increase, I expect that the freshwater injection rate will increase (mainly via ice faster ice shelf breakup and underwater melt) and sea ice area will increase. This experiment will be playing out over the next years and decades," said Hansen in an email to the Post.
Anders Levermann, a climate scientist at the Potsdam Institute for Climate Impact Research, noted that it was "curious" that the feedback loop "is occurring now, after 10,000 years of stability, while we are ramping up the temperature of the planet."
"Trying to dismiss the idea that it has anything to do with global warming is also very difficult," he told the Scientific American.

Bolstering concerns that so-called "feedback loops" should be considered a legitimate and serious concern, a new study shows that a worrying hypothesis put out just three years ago about the impacts of melting Antarctic ice may already have started coming true.
In a paper published in Science Advances, researchers at the University of Tasmania and other institutions found that the melting of Antarctica's glaciers has begun to trigger a "feedback loop" in which that melting's effects on the oceans cause even more ice sheets to deteriorate, and so on.
Chris Mooney of the Washington Post described the feedback loop phenomenon as "one of the most worrisome predictions about climate change" in an article about the findings.
"What we found is not only a modeling study but is something that we observed in the real ocean," Alessandro Silvano, one of the researchers, told the Post. "Our study shows for the first time actual evidence of this mechanism. Our study shows that it is already happening."
As Common Dreams reported in 2015, NASA climate scientist James Hansen first raised concerns about the feedback loop then. As the Post reports, Hansen explained that the melting of glaciers would create fresh water, blocking cold salt water from sinking to the bottom of the ocean and protecting the ice shelves from melting:
When cold surface water no longer sinks into the depths, a deeper layer of warm ocean water can travel across the continental shelf and reach the bases of glaciers, retaining its heat as the cold waters remain above. This warmer water then rapidly melts the glaciers and the large floating ice shelves connected to them.
The continuous melting cycle could soon begin to cause rapidly-rising sea levels and destructive hurricanes and other storms.
"That would mean loss of all coastal cities, most of the world's large cities and all their history," said Hansen when his paper on the feedback loop theory was released.
Hansen told the Post that the new research "provides a nice small-scale example" of the patterns he predicted.
"If we stay on business-as-usual [greenhouse gas] emissions rates, so that global warming continues to increase, I expect that the freshwater injection rate will increase (mainly via ice faster ice shelf breakup and underwater melt) and sea ice area will increase. This experiment will be playing out over the next years and decades," said Hansen in an email to the Post.
Anders Levermann, a climate scientist at the Potsdam Institute for Climate Impact Research, noted that it was "curious" that the feedback loop "is occurring now, after 10,000 years of stability, while we are ramping up the temperature of the planet."
"Trying to dismiss the idea that it has anything to do with global warming is also very difficult," he told the Scientific American.