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Showing posts with label Methane Gun hypothesis. Show all posts
Showing posts with label Methane Gun hypothesis. Show all posts

Friday, September 6, 2013

Rebuttal to Michael Tobis' unsubstantiated attacks on the work of Shakhova

Posted on 1:03 PM by Unknown

Why the jury's still out on the risk of Arctic methane catastrophe

Can scientists overcome huge uncertainties to pin down how close, or far, we might be to a tipping point?

arctic iceberg
Arctic iceberg. Photograph: Delphine Star/Getty Images
by Nafeez Ahmed, "Earth Insight," The Guardian, September 5, 2013

 About a week ago, climate scientist Michael Tobis wrote a critique of my 'Seven facts about the Arctic methane time bomb' following a twitter exchange with him and Chris Colose, author of an article at Skeptical Science arguing that the core scenario of a new Nature paper by Gail Whiteman et al. on the economic costs of Arctic climate change is extremely unlikely.

Much of this debate kicked off because the said Nature paper advances a hypothetical scenario for an abrupt Arctic methane release over either a decade or several decades of about 50 gigatonnes (Gt), and argues specifically that such a scenario is "likely." My own attempt to understand the literature convinced me that the scenario should be viewed as a serious possibility.

Tobis on the other hand is the latest amongst several scientists offering scathing criticisms of that scenario, which in his own words is "as close to impossible as anything in earth science; actual geophysics refutes it."

He begins with my first point, 1. The 50 Gigatonne decadal methane pulse scenario was posited by four Arctic specialists, and is considered plausible by Met Office scientists.


Tobis writes that the Review of Geophysics paper I cite says
"Arctic thawing may release in excess of 50 GT of C [Carbon], a very serious matter... But Ahmed refers to the paper in support of a very different assertion, that 50 GT of methane would be released... But the paper to which he points says nothing of the sort. I conclude that he doesn't really know what he is talking about. Specifically he has already shown that he is confused about the distinction between methane releases and CO2 releases."
However, the carbon release scenarios from permafrost explored by the paper include both methane and carbon. 

Here's what the paper says:
"The most important determinant of whether release of frozen carbon happens as CO2 or CH4 [methane] is whether decomposition proceeds aerobically or anaerobically... In anaerobic conditions, a greater proportion of soil organic carbon decomposition is released as CH4, although not all of it necessarily reaches the atmosphere."
Following this paragraph, the paper cites several scenarios for large-scale releases from permafrost carbon, including the 50-100 Gt carbon release I mentioned.

Further down, the paper continues:
"Thawing of the terrestrial permafrost will result in CO2 and CH4 emissions on time scales of a few decades to several centuries."
So Tobis is wrong in assuming that the carbon release scenarios the paper is discussing are only CO2 - that isn't specified, so I'd assumed the paper was open on whether the 50-100 Gt emissions were methane or carbon. 

This was a mistake, however. The paper makes clear that although the scenarios are not clear on the precise quantification of carbon dioxide compared to methane releases from permafrost thawing, methane releases would be only be a small percentage of the overall carbon release scenarios explored. So Tobis is ultimately correct - the paper does not back up the specific scenario endorsed as likely by the Nature paper. I stand corrected on that.

Therefore, the plausibility of the specific 50 Gt scenario rises and falls on the credibility of the four Arctic specialists, including Dr. Natalia Shakhova, who came up with the scenario in the first place. That leaves point 1 only half intact, so we're left with:

1. The 50 Gigatonne decadal methane pulse scenario was posited by four Arctic specialists
Tobis unfortunately addresses this with only an ad hominem attack on the expertise of these Arctic specialists:
"Whether we should be acknowledging the 'Arctic specialists' as actually expert is, frankly, the question at hand."
Tobis goes through my other citations of the literature arguing that I am confusing quantities and making unwarranted extrapolations. However, my citations of this literature is simply to clarify that the literature does not rule out potentially dangerous releases of Arctic methane. Does Tobis manage to refute point 2. Arctic methane hydrates are becoming increasingly unstable in the context of anthropogenic climate change and it's impact on diminishing sea ice? No. Arctic methane hydrates are becoming increasingly unstable. I said nothing more, or less, than exactly that.

What about fact 3. Multiple scientific reviews, including one by over 20 Arctic specialists, confirm decadal catastrophic Arctic methane release is plausible?

Tobis concedes "A couple of reviews do give some support to this, but are vague about time scales." He then links to what he describes as a "DOE report." Instead, the link goes through to a Geophysical Research Letters study, which, however, he completely ignores, instead quoting from the original Review of Geophysics paper as follows: 

"The risk of a rapid increase in [methane] emissions is real but remains largely unquantified..." 

And he calls me confused! 

He then argues that there is "plenty of room for acceleration without hitting the cataclysmic level. Further evidence doesn't support the immediacy of that scenario at all."

But the Review of Geophysics paper does NOT say that there is "plenty of room for acceleration without hitting the cataclysmic level" - it says that:
"... significant increases in methane emissions are likely, and catastrophic emissions cannot be ruled out."
The paper does NOT say available evidence "doesn't support the immediacy" of a catastrophic scenario, but rather that "uncertainties are large, and it is difficult to be conclusive about the time scales and magnitudes of methane feedbacks."

As for the Geophysical Research Letters study Tobis links to but ignores, it says:
"... while many deep hydrate deposits are indeed stable under the influence of rapid seafloor temperature variations, shallow deposits, such as those found in arctic regions or in the Gulf of Mexico, can undergo rapid dissociation and produce significant carbon fluxes over a period of decades."
I think my fundamental contention - that the scientific literature recognises the possibility of some sort of catastrophic methane scenario - remains valid. Tobis is right, however, to emphasise that there is very little evidence available on quantifying that possibility.

In response to fact 4. Current methane levels are unprecedented, Tobis says yes, but they are "not climbing rapidly", and therefore this is mere "hype." My intention here was not to suggest that current Arctic methane levels are definitive evidence of a catastrophe already underway, but simply to note that it is wrong to say methane levels are NOT rising. They are, and once again, Arctic specialists are concerned. 

According to Charles Miller of NASA's new research programme, Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE):
"The CARVE science team is busy analyzing data from its first full year of science flights. What they're finding, Miller said, is both amazing and potentially troubling.
'Some of the methane and carbon dioxide concentrations we've measured have been large, and we're seeing very different patterns from what models suggest," Miller said. "We saw large, regional-scale episodic bursts of higher-than-normal carbon dioxide and methane in interior Alaska and across the North Slope during the spring thaw, and they lasted until after the fall refreeze. To cite another example, in July 2012 we saw methane levels over swamps in the Innoko Wilderness that were 650 parts per billion higher than normal background levels. That's similar to what you might find in a large city.'
"Ultimately, the scientists hope their observations will indicate whether an irreversible permafrost tipping point may be near at hand. While scientists don't yet believe the Arctic has reached that tipping point, no one knows for sure. 'We hope CARVE may be able to find that "smoking gun," if one exists,' Miller said."
So while NASA Arctic specialists say Arctic methane levels are "amazing" and "potentially troubling," outside the range of most model predictions, and possibly indicative that "an irreversible permafrost tipping point" is near - a matter which "no one knows for sure" - Tobis wants to interpret all the evidence as "refuting" any need for concern. 

The other problem is that Arctic monitoring is still poor, and might be missing significant methane emissions. As Shakhova and her co-author Igor Semiletov told the New York Times' Andy Revkin:
"It is no surprise to us that others monitoring global methane have not found a signal from the Siberian Arctic or increase in global emissions... The number of stations monitoring atmospheric methane concentrations worldwide is very few. In the Arctic there are only three such stations - Barrow, Alert, Zeppelin - and all are far away from the Siberian Arctic. We are doing our multi-year observations, including year-round monitoring, in proximity to the source. In addition to measuring the amount of methane emitted from the area, we are trying to find out whether there is anything specific about those emissions that could distinguish them from other sources. It is incorrect to say that anyone is able to trace that signal yet."
Most Arctic specialists recognise that there's simply not enough research to justify dismissing the possibility of a catastrophe. That sword cuts both ways, of course - equally, there's not enough research justifying conclusions that we are definitely on the brink of a catastrophe.

On 5. The tipping point for continuous Siberian permafrost thaw could be as low as 1.5 C, Tobis concedes this "is on the table," but that "it has nothing to do with undersea methane." Um, I never said it had anything to do with undersea methane.

On 6. Arctic conditions during the Eemian interglacial lasting from 130,000 to 115,000 years ago are a terrible analogy for today's Arctic, he writes: "as a response to Chris Colose" this is a "terrible" response, "because Colose is not relying on the Eemian but on the early Holocene as the analogous period." Yes, Colose does refer to the early Holocene, but he also repeatedly refers to the Eemian, the "Last Interglacial period between 130,000 to 120,000 years ago." In a previous article, I'd already mentioned that in the early Holocene, the East Siberia Arctic Shelf (ESAS) was "not an underwater shelf but a frozen landmass" as reason to be sceptical that paleoclimate data provide a ready analogue for the present.

Tobis then launches an ad hominem attack on climate scientist Paul Beckwith, whom I quoted for this article, and whom Tobis refers to as:
"'Prof' Paul Beckwith, the 'Professor Beckwith' who is a grad student at Ottawa U."
For the record, earlier this year, Beckwith formally passed his PhD examination on abrupt Arctic climate change at the Laboratory for Paleoclimatology and Climatology, University of Ottawa, where he is currently a part-time professor in climatology. Rather than addressing Prof Beckwith's argument, Tobis wants to demean his reputation and ignore his argument (which he fails to refute). Beckwith's full response to Colose is here. Among Beckwith's points, he argues that neither the early Holocene nor Eemian offer good analogues for the present Arctic:
"Earth tilt was larger, so Winter Northern Hemispheric solar radiation was about 40 W/m2 lower than today at 60 degrees North. Thus, the ice formed much more quickly and much thicker in the winter back then. Also, at night much more heat was radiated out to space in the lower GHG world then as compared to our 400 ppm levels today... the summertime Arctic is not believed to be seasonally ice free during these periods. The last time this happened was likely 2 or 3 million years ago... Colder winters in the early Holocene and Last Interglacial and much colder nights (in summers and winters then) meant much thicker and extensive ice formation in winters, and slower melting at night, respectively."
If I was to take Tobis' approach, I could have noted that Chris Colose is a "grad student" at the University of Albany. I didn't, because it's irrelevant.

Finally, Tobis takes on fact 7. Paleoclimate records will not necessarily capture a large, abrupt methane pulse with the following obfuscation: "Now, we swing back to saying that it HAS occurred in the recent geological past, indeed at the time which Colose says is the better analogy." 

This is incorrect. Here, I merely point to a paper in Science by Nisbet which argues specifically that the cold Younger Dryas was ended due to methane emissions which came mostly from wetlands, but for which the initial trigger could have been Arctic methane clathrates:

"A possible explanation for the sudden end of the Younger Dryas is that, at a time of high Arctic insolation, an initial outburst of methane - perhaps from a geological source such as methane clathrates - triggered global warming, initiating both strong wetland emission in the tropics and north (8), and further hydrate responses as the thermal shock penetrated the permafrost (9, 10), freeing methane from decomposing clathrate hydrates and releasing gas pools trapped beneath them."
The evidence for this, however, is inconclusive, so the paper concludes: "The jury thus remains out on the initial trigger..."

On the issue of whether paleoclimate records will actually capture a large, abrupt methane pulse such as the scenario proposed by Shakhova et al., as this paper in Earth and Planetary Science Letters observes, "rapid methane perturbations in the atmosphere are strongly smoothed in ice core records" due to "the relatively short atmospheric lifetime of methane." So it is quite possible that an abrupt, catastrophic methane release of the sort Shakhova proposes has happened, but is undetected in ice cores.

Tobis then declares a "scientific consensus has been reached" that Shakhova's scenario is "implausible in the extreme."

But the scientific consensus amongst ESAS experts is quite different, as I'd already noted. A peer-reviewed study by 20 Arctic specialists of ESAS data from 1995-2011, drawing of course also on Shakhova's work, specifically recognises:
"The emission of methane in several areas of the [ESAS] is massive to the extent that growth in the methane concentrations in the atmosphere to values capable of causing a considerable and even catastrophic warning on the Earth is possible."
It seems clear to me that the scientific literature on the danger of an Arctic methane catastrophe recognises the possibility unequivocally, but highlights huge uncertainty in our knowledge of the processes at work. Most of the literature I've been able to find on this subject shows great humility - and while acknowledging the possibility of worst-case scenarios, makes quite clear that the likelihood of those scenarios is very difficult to gauge.

The Nature paper by Whiteman et al. went too far in stating the Shakhova et al. scenario as "likely." But on the other end of the spectrum, in the comments to his own blog, Tobis hints that Shakhova et al. are involved in "junk science" - despite the fact that their papers have been published in peer-reviewed journals (their 50 Gt scenario is discussed in this paper originally published in the Proceedings of the Russian Academy of Sciences), and that their general thesis is taken seriously by the US National Science Foundation.

Tobis also refers to a response to the Whiteman paper submitted to Nature (though not yet published) by Nisbet et al., which argues that Shakhova's scenario is "improbably large" as there is no evidence for such events during past "glacial/postglacial transitions."

This is certainly a notable contribution to the debate, but if past paleoclimate conditions are not a good analogue for present Arctic conditions - a matter which remains a matter of scientific debate - and if ice cores would not record such a rapid scenario, then the central argument of this paper may be questionable.

Indeed, a 2007 Royal Society paper by NASA scientist Drew Shindell backs this up:
"... the rarity of palaeoclimate evidence for hydrate-induced climate changes argues that this is a fairly unlikely candidate for near-term sudden climate change. Unlike the others, however, anthropogenic climate change may alter the probability of hydrate release when compared with the past, making the overall probability of near-term release extremely difficult to estimate...
Massive methane release by hydrates or from peats also seems to have been extremely rare in the past, but could become more probable in the future world under the influence of anthropogenic forcing. However, at present, it is not possible to judge the probability for such changes reliably."
Shindell's argument offers a warning that lack of past evidence is not a reason for present complacency where anthropogenic forces are changing the climate in ways not necessarily captured by paleoclimate evidence. 

So where does this leave us with regard to the risk of abrupt, catastrophic methane releases? As far as I can discern, the literature is largely agnostic about it, emphasises that specific scenarios are difficult to quantify, and calls for further research. The Review of Geophysics paper, for instance, far from asserting that a catastrophic methane release is refuted by geophysical evidence - as Tobis says - concludes:

"A significant increase in CH4 emissions and atmospheric concentrations due to climate change is therefore a possible scenario for the next century. However, uncertainties are very large, and as discussed above, it is difficult to be very conclusive regarding the magnitude of CH4 feedbacks and their time scales."
What about Shakhova et al.'s specific scenario of a potential 50 Gt methane release at any time (the basic contours of her argument are outlined here, no paywall)? Shakhova et al. say simply that the scenario should be taken seriously as a possibility underscoring the importance of further ESAS research. The fact that Nature co-author Prof Peter Wadhams, who heads up polar ocean physics at Cambridge, also takes it seriously, is significant. Is Prof Wadhams' expertise also to be attacked? Ultimately, in my view, Tobis fails to show either that this scenario specifically, or abrupt methane catastrophe more generally, are unlikely. 

In particular, his claim that there is a scientific consensus demonstrating near impossibility of a risk of a catastrophic methane event strikes me as unsupportable. Disagreement among scientists over the Arctic methane question is real, and it seems clear that Arctic specialists - Shakhova included - largely agree that while catastrophe is possible, more research is needed to discern how likely or unlikely it might be.

While other scientists, many reputable, argue importantly that such scenarios are beyond the pale, to my mind Tobis' egregious ad hominems against Arctic scientists whom he disagrees with have no place in scientific debate.

Dr Nafeez Ahmed is executive director of the Institute for Policy Research & Development and author of A User's Guide to the Crisis of Civilisation: And How to Save It among other books. Follow him on Twitter @nafeezahmed

http://www.theguardian.com/environment/earth-insight/2013/sep/05/jury-out-arctic-methane-catastrophe-risk-real

In response to a comment, Dr. Ahmad wrote:

The simple purpose of my articles on the Arctic methane question have been to investigate whether the scientific literature bears out the possibility of a catastrophe. Apart from the fact this issue is obviously of interest to anyone, my own particular interest in the issue is related to how such an event would impact our societies, economies and geopolitics. 

Of course, I'm not an expert on this issue. Anyone can see that from my bio. Should that prevent me from trying to understand and engage with it?

It's mistaken to think that I am disrespecting the scientist bloggers who think Shakhova's scenario specifically and an abrupt methane catastrophe scenario generally have negligible probability. While these scientist bloggers have articulated their views very well, the reality is that there are lots of other scientists - their views being expressed in the literature - who argue that we cannot rule out such scenarios, and that we cannot even know for sure how likely or unlikely they are.

Now Semiletov and Shakova are clearly at the forefront of research on the East Siberian Arctic Shelf (ESAS), and are the main people arguing that the ESAS harbours a unique danger of abrupt climate change due to conditions not found anywhere else on the planet. 20 Arctic specialists agree with them.

Perhaps they are wrong, and the scientist bloggers critiquing them are right. But I don't know that, and looking at the peer-reviewed literature, I cannot see any arguments which support the idea that Shakhova is talking complete nonsense. Yes, there have been several of blog posts by scientists and science students suggesting this - but all the peer-reviewed analyses of the question of Arctic methane risks by leading scientists in the field show that there is a possible danger here which cannot be quantified.

Now Tobis is openly arguing, effectively, that Shakhova and her colleagues are non-experts, and that they offer no evidence for their claims. So who is disrespecting scientists, really? As a mere journo trying to get to the bottom of this, as a mere HUMAN trying to get to the bottom of this, I'm genuinely trying to understand how Tobis and others can insist Shakhova et al. offer ZERO evidence at all. How can they be permitted to deliver papers at scientific conferences, how can they be publishing in peer-reviewed journals (and I note that their 50 Gt abrupt methane release scenario was also peer-reviewed too) if all they are doing is junk science? Shakhova is repeatedly arguing that significant portions of the ESAS is underlain by methane gas hydrates which are relatively shallow and vulnerable to destabilisation, based on direct observation and sampling. Is she lying? Is she deluded? And are the Arctic specialists reviewing her and others' ESAS research who think there is something to their findings also deluded and/or liars?

I just find this really difficult to believe. It doesn't seem credible to me that Shakhova et al. and the Arctic scientists who support them/consider them credible - many of them leading experts in the field too - are just talking nonsense and junk science combined with unwarranted speculation. If that's the case, how the hell are they getting published in leading science journals? And why do so many Arctic specialists agree with them? Prof Peter Wadhams from Cambridge told me that there is a relative consensus on the possibility of danger amongst ESAS experts. Is he just lying too? Or deluded?

If that IS happening, then there is a fundamental problem with the scientific process here, Shakhova et al. need to be put in their place, and we should all be worried about how a large number of Arctic specialists can be taken in by complete speculative nonsense.

From my perspective, I see two sets of experts - most Arctic specialists themselves, who will not rule out the possibility that Shakhova might be right and who respect her work - and a lot of non-Arctic experts who, however, may well have expertise in methane hydrates generally or climate modelling, who find Shakhova's arguments far-fetched and evidence-thin. 

It's in this context of disagreement that I've tried to see what the peer-reviewed literature itself says, and I've tried to let the lit speak for itself as much as is possible here. I don't see any lit which proves any scientific consensus demolishing Shakhova et al. 

Readers are encouraged to do their own research and make up their own minds, and yes of course, to read up on my links (please don't tell me you like reading blogs hoping for gospel truth - the links are there to be read and checked as supporting evidence!) and if you disagree with my conclusions, the key thing that would help me is to see how and why Shakhova et. al are not actually providing compelling evidence for their arguments. 

I won't be able to respond further for a while as I'm away, but will read constructive comments with interest.
 
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Posted in East Siberian Arctic Shelf, Eemian, Holocene thermal maximum, Igor Semiletov, Methane Gun hypothesis, Methane hydrates, Michael Tobis, Natalia Shakhova, Peter Wadhams | No comments

Wednesday, July 31, 2013

Methane hydrates: a volatile time bomb in the Arctic

Posted on 7:52 AM by Unknown

Gpkgyj67-1349405231Methane locked under the Arctic ice could take climate change to a whole new level. Antonio Delgado Huertas 

by Antonio Delgado Huertas, The Conversation, October 17, 2012

The risk with climate change is not with the direct effect of humans on the greenhouse capacity of Earth’s atmosphere. The major risk is that the relatively modest human perturbation will unleash much greater forces. The likelihood of this risk is intimately tied to the developments over the next decade in the Arctic. Accelerating ice loss and warming of the Arctic is disturbing evidence that dangerous climate change is already with us. As I have argued earlier, now that we have realised this our efforts should be directed at managing the situation in the Arctic and avoiding the spread of dangerous climate change elsewhere.


The Arctic is a core component of the earth system. Six of the 14 climate change tipping points of the earth system are located in the Arctic region.
Whereas the term tipping point was initially introduced to the climate change debate in a metaphoric manner, it has since been formalised and introduced in the context of systems exhibiting rapid, climate-driven change, such as the Arctic. Tipping points have been defined in the context of earth system science as the critical point in forcing at which the future state of the system is qualitatively altered.
Tipping elements are defined, accordingly, as the structural components of the system directly responsible for triggering abrupt changes once a tipping point is passed. This is because they can be switched into a qualitatively different state by small perturbations.



Of the many tipping elements in the Arctic, that with potentially greatest consequences if perturbed is the vast methane deposit. Methane is a greenhouse gas. A molecule of methane has 20 times the greenhouse effect of a CO₂ molecule, and the release of methane has been linked to climatic transitions along the history of planet Earth.
The Arctic contains vast reserves of methane stored as methane hydrate, a gel-like substance formed by methane molecules trapped in frozen water. The methane hydrate deposits are estimated at between 1,000 and 10,000 Gigatons (109 tons) of CO₂-equivalents as methane, much of which is present in the shallow sediments of the extensive Arctic shelves. This amount of greenhouse gas is several times the total CO₂ release since the industrial revolution.
Even moderate (a few degrees C) warming of the overlying waters may change the state of methane from hydrates to methane gas, which would be released to the atmosphere. If this release is gradual, methane will add a greenhouse effect to the atmosphere. This will only be temporary, as it will be oxidised to CO₂, with a decline in the greenhouse effect of 20-fold per unit carbon.
However, if the state shift is abrupt it may lead to a massive release of methane to the atmosphere, which could cause a climatic jump several-fold greater than the accumulated effect of anthropogenic activity.

Data collected on a recent cruise confirm methane is being emitted. Antonio Delgado Huertas

Recent assessments have found bubbling of methane on the Siberian shelf. Models suggest that global warming of 3 °C could release between 35 and 94 Gt C of methane, which could add up to an additional 0.5 °C of global warming. Moreover, frozen soils and sediments contain large amounts of methane hydrates that can be released to the atmosphere. Indeed, rapid thawing of the Arctic permaforst has been reported to lead to the release of large amounts of methane.
In our most recent cruise this summer (June 2012) along the Fram Strait and Svalbard Islands we found concentrations of methane in the atmosphere of about 1.65 ppm. However our equilibrium experiments (air atmospheric with Arctic surface water) reached values that were generally between 2.5 ppm and 10 ppm, with maximum values up to 35 ppm. These results confirm that this area of the planet is emitting large amounts of methane into the atmosphere.
Understanding and forecasting the response of Arctic methane hydrate deposits to rapid warming and thawing in the Arctic is of the utmost importance.
Provided the magnitude of these risks, and those associated with other tipping elements in the Arctic, our collective response to climate change appears to be a careless walk on the razor edge.
https://theconversation.com/methane-hydrates-a-volatile-time-bomb-in-the-arctic-9891
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Posted in Arctic Methane Emergency Group, Methane Gun hypothesis, Methane hydrates | No comments

Saturday, July 27, 2013

Extended interview with Natalia Shakhova by Nick Breeze at the 2012 European Geophysical Union meeting

Posted on 6:08 PM by Unknown
http://vimeo.com/71177231  Igor Semiletov can be heard in the background.
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Posted in Igor Semiletov, Methane Gun hypothesis, Natalia Shakhova | No comments

RL Miller: The Truth Behind That $60 Trillion Climate Change Price Tag

Posted on 3:49 PM by Unknown
The fallout from a recently-published article has some climate scientists questioning the validity of the numbers

Methane

An iceberg carved from a glacier floats in the Jakobshavn fjord in southwest Greenland. (Photo: Konrad Steffen / Reuters)

by R.L. Miller, TakePart, July 27, 2013

This week, news broke that if all [actually, 50 Gt is about 3.5-5.0% of the methane estimated to lie below the subsea permafrost of the Eastern Siberian Arctic Shelf: see article with Shakhova interview included at this link: http://thinkprogress.org/climate/2012/01/19/406762/arctic-methane-outgassing-on-the-east-siberian-shelf-primer-interview-dr-natalia-shakhova/] the methane off the East Siberian seafloor was released, the fallout would cost $60 trillion — a huge, staggering number.

For comparison’s sake, the world’s GDP is $70 trillion. The findings assume that 50 gigatons of methane would be released over the course of 10 to 20 years in a warming pulse.

Some climate scientists disagree with the underlying assumption. Gavin Schmidt has taken to Twitter to argue that 50 gigatons is an excessive estimate; prior warming periods didn’t show similarly large releases of methane.

On the other hand, climate scientist Dr. Michael Mann tells TakePart: “The precise magnitude [of methane] is an object of valid debate, but the possibility of a substantial release cannot be dismissed out of hand.” Climate modelers have underestimated Greenland sheet ice and Arctic sea ice melt, so the estimate is not outside the realm of possibility.


The authors make it clear that they’re responding to exuberant claims of $100 billion in short term benefits from a warming Arctic — if the sea ice melts, trade routes will be shortened. Neither the World Economic Forum (WEF) in its Global Risk Report, nor the International Monetary Fund in its World Economic Outlook, recognizes the potential economic threat from changes in the Arctic.
 
Very large numbers make us sit up and take notice, but they’re also hard to grasp. What is climate change currently costing even without that warming pulse? A NRDC report estimates that American taxpayers, through the federal government, paid $100 billion in 2012 — more than the cost of education or transportation. (And that doesn’t include what state and local governments, insurers, or private citizens paid.) Mann estimates the global cost at $1.4 trillion per year in coastal damage, droughts, fires, floods and hurricanes.

We know that Mayor Bloomberg’s proposal to armor New York City to protect against the next Sandy has a $20 billion price tag. No similar grand proposal has been made for other great cities of the East Coast — Boston, Washington, D.C., or Charleston. No similar proposal has been made for Midwestern cities facing floods, or Southwestern cities, where wildfire season now starts July 1 and ends June 30.

And what of Miami? It contributed $263 billion to gross domestic product in 2010, according to the Bureau of Economic Advisors. Caught between rising seas to the east and the Everglades to the west, the city is doomed to drown.

Abandoning Miami means not only moving or abandoning the businesses who create its gross domestic product, but walking away from its pricey real estate, its roads, hospitals, schools and infrastructure. The cost of relocating its people needs to be calculated both in dollars and in heartbreak. But if you ask people to estimate the cost of abandoning Miami, you get blank stares. It’s as if the language to ask the question hasn’t been invented yet.

“It is not difficult to envision much larger costs, [i.e., $60 trillion] given the potential larger and more abrupt warming [the more abrupt the warming, the more costly it is to try to adapt] that the authors calculate,” says Mann. And it’s not difficult to imagine that there are costs we haven’t even begun to imagine. And when you multiply those costs, city after city after city, suddenly $60 trillion becomes a very realistic and frightening number.

http://www.takepart.com/article/2013/07/26/methane-climate-change-arctic-60-trillion
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Posted in Arctic Methane Emergency Group, Jakobshavn Isbræ, Methane Gun hypothesis, Methane hydrates | No comments

Eemian interglacial period poor analog for current Arctic warming

Posted on 2:18 PM by Unknown

Warm climate -- cold Arctic? The Eemian is a poor analogue for current climate change


by phys.org, June 14, 2012

The Eemian interglacial period that began some 125,000 years ago is often used as a model for contemporary climate change. In the international journal Geophysical Research Letters, scientists from Mainz, Kiel and Potsdam, Germany, now present evidence that the Eemian differed in essential details from modern climatic conditions.

To address the question about how climate may develop in the future, earth scientists direct their attention to the past. They look for epochs with similar conditions to today. The major identified climatic processes are then simulated with numerical models to further test possible reactions of the Earths' system. An epoch which is often regarded suitable for such an undertaking is the Eemian warm period, which began around 125,000 years ago following the Saalian ice age.
For about 10,000 years, average temperatures on Earth in the Eemian were rather enhanced – probably several degrees above today's level. This seems to be well documented in both ice cores as well as terrestrial records from land vegetation. Substantial parts of the Greenland ice had melted, and global sea level was higher than today. "Therefore, the Eemian time is suited apparently so well as a basis for the topical issue of climate change", says Dr Henning Bauch, who works for the Academy of the Sciences and the Literature Mainz (AdW Mainz) at GEOMAR | Helmholtz Centre for Ocean Research Kiel.
However, in a study which appears in the recent issue of the international journal Geophysical Research Letters Dr Bauch, Dr Evgeniya Kandiano of GEOMAR as well as Dr Jan Helmke of the Institute for Advanced Sustainability Studies in Potsdam now show that the Eemian warm period differed from the present day situation in one critical aspect – the development in the Arctic Ocean.
In our current warm period, also called Holocene, oceanic and atmospheric circulation delivers large amounts of heat northward into the high latitudes. The most well known heat conveyer is the Gulf Stream and its northern prolongation called the North Atlantic Drift. The currents provide not only the pleasant temperatures in Northern Europe, they also reach as far as the Arctic. Studies in the last years have shown that the oceanic heat transport to the Arctic has even increased, while the summer sea ice cover in the Arctic Ocean seems to be decreasing continuously. It has long been assumed that such conditions also prevailed 125,000 years ago. Accordingly, the Arctic should have been by and large ice-free in the Eemian summers.
Dr Bauch's group examined sediment cores from the seabed in which information about the climate history of the past 500,000 years is stored. These come from the Atlantic to the west of Ireland and from the central Nordic Seas to the east of the island of Jan Mayen. The sediments contain minute calcite tests of dead microorganisms (foraminifers). "The type of species assemblage in the respective layers as well as the isotopic composition of the calcitic tests give us information about temperature and other properties of the water in which they lived at that time", explains Dr Bauch.
The samples from the Atlantic delivered the higher-than-Holocene temperature signals so typical for the Eemian. The tests from the Nordic Seas, however, tell quite another story. "The found foraminifers of Eemian time indicate comparatively cold conditions." The isotope investigations of the tests, in combination with previous studies of the group, "indicate major contrasts between the ocean surfaces of these two regions ", according to Dr Bauch. "Obviously, the warm Atlantic surface current was weaker in the high latitude during the Eemian than today." His explanation: "The Saalian glaciation which preceded the Eemian was of much bigger extent in Northern Europe than during the Weichselian, the ice age period before our present warm interval. Therefore, more fresh water from the melting Saalian ice sheets poured into the Nordic Seas, and for a longer period of time. This situation had three consequences: The oceanic circulation in the north was reduced, and winter sea ice was more likely to form because of lower salinity. At the same time, this situation led to a kind of 'overheating' in the North Atlantic due to a continuing transfer of ocean heat from the south."
On the one hand, the study introduces new views on the Eemian climate. On the other hand, the new results have consequences for climatology in general: "Obviously, some decisive processes in the Eemian ran off differently, like the transfer of ocean warmth towards the Arctic. Models should take this into consideration if they want to forecast the future climate development on the basis of past analogues like the Eemian ", says Dr. Bauch.
http://phys.org/news/2012-06-climate-cold-arctic-eemian.html
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Posted in Arctic Ocean, Eemian, Methane Gun hypothesis, Methane hydrates, Ocean temperatures | No comments

Methane gas likely spewing into the oceans through vents in sea floor

Posted on 10:07 AM by Unknown

Could speed up global warming more efficiently than carbon dioxide

by Denise Brehm, Civil and Environmental Engineering, MIT News, September 2, 2009


Scientists worry that rising global temperatures accompanied by melting permafrost in arctic regions will initiate the release of underground methane into the atmosphere. Once released, that methane gas would speed up global warming by trapping the Earth's heat radiation about 20 times more efficiently than does the better-known greenhouse gas, carbon dioxide.

An MIT paper that appeared online August 29, 2009, in the Journal of Geophysical Research elucidates how this underground methane in frozen regions would escape and also concludes that methane trapped under the ocean may already be escaping through vents in the sea floor at a much faster rate than previously believed. Some scientists have associated the release, both gradual and fast, of subsurface ocean methane with climate change of the past and future.

graphic
The image above depicts underground methane gas as it begins to invade fine-grain sediment (shown in yellow) by creating a fracture. In the image at right, the blue circles represent pore spaces where the gas has invaded. RUBEN JUANES

"The sediment conditions under which this mechanism for gas migration dominates, such as when you have a very fine-grained mud, are pervasive in much of the ocean as well as in some permafrost regions," said lead author Ruben Juanes, ARCO Assistant Professor in Energy Studies in the Department of Civil and Environmental Engineering.
ruben-juanes
Ruben Juanes, the ARCO Assistant Professor in Energy Studies. CHRIS CHURCHILL

"This indicates that we may be greatly underestimating the methane fluxes presently occurring in the ocean and from underground into Earth's atmosphere," said Juanes. "This could have implications for our understanding of the Earth's carbon cycle and global warming."

Methane, the primary component of natural gas, is more abundant in the Earth's atmosphere now than at any time during the past 400,000 years, according to a recent analysis of air bubbles trapped in ice sheets. Over the last two centuries, methane concentrations in the atmosphere have more than doubled. It is estimated that about 60 percent of global methane emissions are tied to human activities like raising livestock and coal-mining, with the rest tied to natural sources such as wetlands, decomposing forests and underground deposits known as methane hydrates.

In the hydrate phase, a methane gas molecule is locked inside a crystalline cage of frozen water molecules. These hydrates exist in a layer of underground rock or oceanic sediments called the hydrate stability zone or HSZ. Methane hydrates will remain stable as long as the external pressure remains high and the temperature low. Beneath the hydrate stability zone, where the temperatures are higher, methane is found primarily in the gas phase mixed with water and sediment.

But the stability of the hydrate stability zone is climate-dependent.

If atmospheric temperatures rise, the hydrate stability zone will shift upward, leaving in its stead a layer of methane gas that has been freed from the hydrate cages. Pressure in that new layer of free gas would build, forcing the gas to shoot up through the HSZ to the surface through existing veins and new fractures in the sediment. A grain-scale computational model developed by Juanes and recent MIT graduate Antone Jain indicates that the gas would tend to open up cornflake-shaped fractures in the sediment, and would flow quickly enough that it could not be trapped into icy hydrate cages en route.

"Previous studies did not take into account the strong interaction between the gas-water surface tension and the sediment mechanics. Our model explains recent experiments of sediment fracturing during gas flow, and predicts that large amounts of free methane gas can bypass the HSZ," said Juanes.

Using their model, as well as seismic data and core samples from a hydrate-bearing area of ocean floor (Hydrate Ridge, off the coast of Oregon), Juanes and Jain found that methane gas is very likely spewing out of vents in the sea floor at flow rates up to 1 million times faster than if it were migrating as a dissolved substance in water making its way through the oceanic sediment - a process previously thought to dominate methane transport.

"Our model provides a physical explanation for the recent striking discovery by the National Oceanic and Atmospheric Administration of a plume 1,400 meters high at the seafloor off the Northern California Margin," said Juanes. This plume, which was recorded for five minutes before disappearing, is believed not to be hydrothermal vent, but a plume of methane gas bubbles coated with methane hydrate.

The Jain and Juanes paper in the Journal of Geophysical Research also explains the short-term consequences of injecting carbon dioxide into the ocean's subsurface, a method proposed by some researchers for reducing atmospheric greenhouse gas. Juanes found that while some of the CO2 would remain trapped as a hydrate, much would likely spew up through fractures just as methane does.

"It is important to keep both methane and carbon dioxide either in the pipeline or underground, because the consequences of escape can be quite dangerous over time," said Juanes.

This research was funded by the U.S. Department of Energy.

http://web.mit.edu/newsoffice/2009/methane-0902.html

Ruben Juanes

ARCO Associate Professor in Energy Studies

I am a geoscientist with a strong interest in the physics of multiphase flow in porous media.

My research focuses on advancing our fundamental understanding and predictive capabilities of the simultaneous flow of two or more fluids through rocks, soils and other porous materials.

Research in my group combines theory, simulation and experiments that elucidate fundamental aspects of multi-fluid flow, which we then apply for prediction of large-scale Earth science problems in the areas of energy and the environment, including geological carbon sequestration, methane hydrates, and ecohydrology of arid environments.
Loosely speaking, our research areas are:
  • Methane: methane hydrates in nature; methane venting from freshwater sediments
  • CO2: Geological carbon sequestration; capillary and solubility trapping; geomechanics
  • Oil: Enhanced oil recovery; flow instabilities; mixing; flow through fractured media
  • Water: Water infiltration; gravity fingering; ecohydrology of arid environments
I teach courses in soil mechanics (undergraduate), groundwater hydrology (graduate) and computational methods for flow in porous media (advanced graduate). My current teaching schedule is:
  • Spring 2013:
    • 1.723: Computational Methods for Flow in Porous Media (stellar website)
  • Previous semesters:
    • 1.035: Structural and Soil Mechanics (stellar website)
    • 1.72: Groundwater Hydrology (stellar website)
  • Courses at other institutions
    • PGE383: Computational Geomechanics (UT Austin)
    • PE120: Fundamentals of Petroleum Engineering (Stanford)
    • PE224: Advanced Topics in Reservoir Simulation (Stanford)
    • PE260: Environmental Aspects of Petroleum Engineering (Stanford)
    • PE281: Applied Mathematics in Reservoir Engineering (Stanford)
    • E77: Introduction to Computer Programming for Scientists and Engineers (UC Berkeley)
    • CE100: Elementary Fluid Mechanics (UC Berkeley)
For other academic activities and a complete list of publications, see my complete CV.
http://juanesgroup.mit.edu/juanes
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Posted in Arctic Methane Emergency Group, Methane Gun hypothesis, Methane hydrates | No comments
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