http://dotearth.blogs.nytimes.com/2010/03/05/the-heat-over-bubbling-arctic-methane/

"there is no evidence (yet) that what is happening is fundamentally
new or destabilizing"

On Mar 5, 10:11 pm, John Nissen <[email protected]> wrote:
> http://www.worldchanging.com/archives/011011.htmlMethane Melt: The Most 
> Important Story You Don't FollowAlex Steffen, 5 Mar 10
> We've written before about the danger that climate change will lead to the 
> thawing and release of methane frozen on the ocean floor, and indeed the 
> worrisome news that some scientists were observingpatches of Arctic sea 
> foaming with gas bubbles from "methane chimneys" rising from the sea floor.
> Now, researchers in Alaska have founda similar process underway:
> Natalia Shakhova, a scientist at the university and a leader of the study, 
> said it was too soon to say whether the findings suggest that a dangerous 
> release of methane looms. In a telephone news conference, she said 
> researchers were only beginning to track the movement of this methane into 
> the atmosphere as the undersea permafrost that traps it degrades.
> But climate experts familiar with the new research reported in Friday’s issue 
> of the journal Science that even though it does not suggest imminent climate 
> catastrophe, it is important because of methane’s role as a greenhouse gas. 
> Although carbon dioxide is far more abundant and persistent in the 
> atmosphere, ton for ton atmospheric methane traps at least 25 times as much 
> heat.
> Until recently, undersea permafrost has been little studied, but work so far 
> shows it is already sending surprising amounts of methane into the 
> atmosphere, Dr. Shakhova and other researchers are finding.
> Last year, scientists from Britain and Germany reported that they had 
> detected plumes of methane rising from the Arctic seabed in the West 
> Spitsbergen area, north of Scandinavia. At the time, they said they had begun 
> their work hoping to gain data to predict future emissions and had not 
> expected to find evidence that the process was under way.
> It is “indispensable” to keep track of methane in the region, Martin Heimann 
> of the Max Planck Institute in Germany said in a commentary accompanying the 
> Science report. So far, Dr. Heimann wrote, methane contributions from Arctic 
> permafrost have been “negligible.” He added: “But will this persist into the 
> future under sustained warming trends? We do not know.”
> In an e-mail message, Euan G. Nisbet of the University of London, an expert 
> on atmospheric methane, said the situation “needs to be watched carefully.”
> Atmospheric concentrations of methane have more than doubled since 
> pre-industrial times, Dr. Heimann wrote. Most of it comes from human 
> activities including energy production, cattle raising and the cultivation of 
> rice. But about 40 percent is natural, including the decomposition of organic 
> materials in wetlands and frozen wetlands like permafrost.
> Dr. Shakhova said that permafrost in the East Siberian Arctic Shelf, peat 
> land that flooded as sea levels rose after the last ice age, is degrading in 
> part because runoff from rivers that feed the Arctic Ocean is warmer than in 
> the past.
> She estimated that annual methane emissions from the East Siberian Arctic 
> Shelf total about seven teragrams. (A teragram is 1.1 million tons.) By some 
> estimates, global methane emissions total about 500 teragrams a year.
> Dr. Shakhova said that undersea methane ordinarily undergoes oxidation as it 
> rises to the surface, where it is released as carbon dioxide. But because 
> water over the shelf is at most about 50 meters deep, she said, the gas 
> bubbles to the surface there as methane. As a result, she said, atmospheric 
> levels of methane over the Arctic are 1.85 parts per million, almost three 
> times as high as the global average of 0.6 or 0.7 parts per million. 
> Concentrations over the shelf are 2 parts per million or higher.
> A huge release of one-frozen methane is (potentially) almost the definition 
> of afeedback loop, perhaps even a tipping point into runaway climate change.
> Luckily, we're not there yet. Scientists have been very clear to say that 
> while these field observations are surprising and disturbing, they do not yet 
> indicate a catastrophe. We need to wait for more data to figure out if it's 
> time to panic yet.
> In the meantime, we need to focus even more strongly on four solution spaces:
> 1) Getting to azero net emissionseconomy as quickly as possible. It's very 
> clear now that we can do this at a net gain for society, with more (and more 
> wide-spread) prosperity for most people, and that it's largely the opposition 
> of entrenched interests that's preventing us from making huge strides 
> forward: this needs to change.
> 2) Implementingclimate-adaptive ecological restoration, safeguardingecosystem 
> services and researchingsoil carbon sequestrationand other practices that 
> have multiple benefits while pulling greenhouse gasses from the air. We need 
> to be helping the planet's natural systems heal towards resilience as much as 
> we possibly can.
> 3) Engaging ina stronger and more realistic debate about geoengineering, its 
> limits and its politics, especially since news of potential tipping points 
> always accelerates calls for geoengineering research, even deployment. 
> Geoengineering's main use in the climate debate at the moment is as 
> apropaganda tool by those seeking to stall action on emissions reduction; 
> that doesn't mean that we don't need to discuss what mega-scale answers might 
> be possible should we find tipping points sliding past more quickly than we 
> feared.
> 4)Building psychological resiliencein the face of huge and alarming planetary 
> changes. News like this is disturbing. We need to find ways, as a culture, as 
> communities and as individuals, to understand disturbing changes without 
> losing our balance. Psychologically wrecked people are no good to themselves, 
> others or the planet. We need to promote the capacity to be healthy and happy 
> despite monumental challenges.

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