Humanity faces 70 feet of sea level rise, possibly coming much sooner than has been expected if we continue with unrestricted carbon pollution. Two recent studies underscore our perilous situation.
The first study found, âEast Antarcticaâs Ice Sheet Not as Stable as Thought,â as Science reported. This conclusion is consistent with other recent research that found weâre all but certain to end up with a coastline at least this flooded (20 meters or 70 feet):
Some have taken solace in the notion that this amount of sea level rise might take more than a thousand years. But a second study finds, âstretches of ice on the coasts of Antarctica and Greenland are at risk of rapidly cracking apart and falling into the ocean.â
The lead author, Jeremy Bassis from the University of Michigan, explained that if this new analysis is right, âwe might be closer to the higher end of sea level rise estimates for the next 100 years.â That âhigher endâ is about 5 or 6 feet.
Hereâs a video of Bassis discussing his findings:
A key point of the study is that current ice sheet models donât capture what is already being observed with our modest 1.5°F warming to date â" 60% faster sea level rise than models had projected:
Iceberg calving, or the formation of icebergs, occurs when ice chunks break off larger shelves or glaciers and float away, eventually melting in warmer waters. Although iceberg calving accounts for roughly half of the mass lost from ice sheets, it isnât reflected in any models of how climate change affects the ice sheets and could lead to additional sea level rise, Bassis said.
âFifty percent of the total mass loss from the ice sheets, we just donât understand. We essentially havenât been able to predict that, so events such as rapid disintegration arenât included in those estimates,â Bassis said. âOur new model helps us understand the different parameters, and that gives us hope that we can better predict how things will change in the future.â
Earlier studies had also found that rapid ice loss is possible. A 2009 study of coral fossils in the journal Nature found âcatastrophic increase of more than 5 centimetres per year over a 50-year stretch is possibleâ â" that is more than 8 feet in half a century. The lead author of that study warned, âThis could happen again.â
The new study provides a mechanism by which such rapid ice loss may be possible. âPortions of Greenland and Antarctica,â the it concludes, âmay be vulnerable to rapid ice loss through catastrophic disintegration.â See also Like Butter: Study Explains Surprising Acceleration Of Greenlandâs Inland Iceâ and Antarctica Is Melting From Below, Which âMay Already Have Triggered A Period of Unstable Glacier Retreatâ.
Letâs return to the study of the East Antarctic Ice Sheet (EAIS) during the Pliocine Epoch (from 5.3 million to 2.6 million years ago). Lead author Carys Cook explained:
âScientists previously considered the East Antarctic ice sheet to be more stable than the much smaller ice sheets in West Antarctica and Greenland, even though very few studies of East Antarctic ice sheet have been carried out. Our work now shows that the East Antarctic ice sheet has been much more sensitive to climate change in the past than previously realised. This finding is important for our understanding of what may happen to the Earth if we do not tackle the effects of climate change.â
Itâs important because, as Science reported, âCurrent warm temperatures and high greenhouse gas conditions are reminiscent of the warm Pliocene Epoch,â when mean temperatures were â2°C to 3°C warmer than today, and atmospheric carbon dioxide concentrations between 350 and 450 parts per millionâ (weâre currently at 400 ppm). And that matters because:
Some data have also suggested that sea levels were perhaps 22 meters higher than todayâ"and even complete melting of the WAIS [West Antarctic ice sheet] and Greenland couldnât account for more than about 12 meters of that, Cook says. Melting of the EAIS would have to have contributed.
Now it appears the EAIS can see significant retreat even with the level of warming we are headed toward in the second half of this century.
Just last year the lead author of paleoclimate research funded by the National Science Foundation (NSF) said, âThe natural state of the Earth with present carbon dioxide levels is one with sea levels about 70 feet higher than now.â And that was only slightly less worrisome than a 2009 paper in Science that found when CO2 levels were this high 15 million years ago, it was 5° to 10°F warmer and seas were 75 to 120 feet higher.
The time to rapidly reduce carbon pollution was decades ago, but now is still vastly better than later.
The post Greenland And Antarctica âMay Be Vulnerable To Rapid Ice Loss Through Catastrophic Disintegrationâ appeared first on ThinkProgress.
Authored by:
Joseph Romm
Joe Romm is a Fellow at American Progress and is the editor of Climate Progress, which New York Times columnist Tom Friedman called "the indispensable blog" and Time magazine named one of the 25 "Best Blogs of 2010." In 2009, Rolling Stone put Romm #88 on its list of 100 "people who are reinventing America." Time named him a "Hero of the Environmentâ³ and âThe Webâs most influential ...
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