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The researchers have revealed that sea temperatures don’t just affect the margins of the large Antarctic ice sheet, but a close connection exists between the Southern Ocean and the interior of the ice sheet, through narrow corridors of fast moving ice, known as ice streams.
“We found that the ice streams, which are like arteries of flowing ice, are capable of triggering rapid, significant changes right through to the interior of the ice sheet,” says Dr Golledge.
Eighty percent of the heat from global warming has been taken up by the ocean and much of this warming is in the Southern Ocean around Antarctica. Present observations show that these warm ocean currents are already melting the marine margin of the ice sheet in the Amundsen Sea, says Dr Golledge.
Made me think... What if someone nuked the hell out of the antarctic?
Originally posted by jonnywhite
There're deep frozen methane patches in the oceans but these have some protection against melting. However, they would be catastrophic (if it isn't already) if they melted. The more immediate worry is the permafrost. And there might be areas of methane too in all that that I don't know about.
Originally posted by poet1b
reply to post by littled16
There is nothing natural about this warming cycle. The historical record shows us this has never happened before so rapidly.
We are about to go on one crazy ride.
On an average summer, about half of Greenland's surface ice melts, according to NASA. This summer, satellites showed about 97 percent of the ice sheet thawed at some point in mid-July.
Originally posted by poet1b
In 2011, Russian scientist discovered plumes of methane coming up out of the Arctic Ocean's continental shelf up to a KM wide. That is something to worry about.
From what I have read, if the Antarctic ice cap melts, we would see a 100' plus increase in ocean levels, 20' if only Greenland melts. It has been awhile since I have looked at the predicted sea level rise, but is enough to put a lot of places underwater.
At this point in time it is hard to say how bad things will get, but they can get very bad.