"I think there is a simpler explanation, and that is that the planetary boundary layer is shallow due to the typical inversion, so CO2
tends to build up near the ground during the non-growing season. My guess is that the late summer values also tend to be a bit lower than Mauna Loa due to the CO2 being pulled out from a thinner layer."
If the planetary boundary layer is shallower during winters and consequently CO2 builds up near the ground during the non-growing season, and the drop in CO2 concentrations follow the summer vegetation plus the CO2 being "pulled out from a thinner layer", how does this interfere with:
(1) the isotopic composition between carbon 12, 13 and 14 isotopes in the Arctic
(2) the ventilation rates of the Arctic air mass with the global air mass. (As I understand the "panning" of Polar air mass by the jet streams reduces ventilation: if the cold air escapes south, the replacement air will bring in globally more balanced or mixed air masses). The global air mass should contain a balaced (or higher) proportion of carbon 14 than permafrost / methane clathrate released (ancient) carbon discharges.
(3) the strong panning of polar vortex induces, or helps, the Arctic ozone hole to form: can this influence methane oxidation rate by ozone? Can hydroxyl reduction be compensated with the higher ozone levels to oxidise the Arctic methane from seabed or permafrost?
Importantly, the entire Eurasian carbon stock may have been diluted 50% by ancient carbon from permafrost, earlier during Holocene. This is because unusually high carbon-14 outliers are found with up to 5,000 extra carbon-14 years in writing materials in China. In air concentration this rate of dilution amounts to one carbon-14 half life, from it hence can be derived that 50% of carbon in the air came out of the ancient permafrost.
To zoom into these processes accurately, if the rising of planetary boundary layer and the panning of air by the polar vortex alter CO2 presence it would be prudent if there were any estimates how much carbon was lost or gained in the ground level as result of these processes and what kind of noise these could produce to the overall carbon-14 dilution process by the permafrost, as well as ozone driven Arctic methane losses.
The situation is very bad: Since 2006 the Arctic warming has been 17 times faster than the stated rate of the observable warming that was recently published in Nature. I will raise this as objection directly to the Prime Minister David Cameron that UK Met Office is totally mistaken in its advices. This is yet another reason why the sea ice disappearance is to be expected 2015 rather than between years 2030 to 2099 and methane follows it.
Regards,
Albert
> Date: Mon, 4 Jun 2012 09:46:25 -0400
> Subject: Re: [geo] 400 ppm and rising
> From: mmac...@comcast.net
> To: S.Sa...@ed.ac.uk; Geoengi...@googlegroups.com
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Hi Albert,
You make an interesting point about the storm surges mixing the water.
This will take warmer surface water down to the seabed - adding to other mixing phenomena that
Shakhova and Semiletov have been observing. They believe it is this
warming that is causing rapid release of methane, whether it is from hydrates
or from free gas previously trapped below subsea permafrost. This is
a mechanism for rapid methane release that David Archer says
does not and cannot exist, see extract from [1]. The Russians estimated that, if one could
imagine the methane release that they were observing from one part of the ESAS
happening continuously over the whole of the ESAS, it would amount to several
gigatonnes of methane per annum [2]. The global warming from that would
quickly dwarf global warming from CO2, and we'd be liable to experience
run-away global warming. One does not need hundreds of Gigatonnes of
methane over a few years to obtain a catastrophe, as Archer maintains, see extract from [1].
A gigaton of methane release per year for a few years could build up to several
Watts per square metre of global climate forcing, compared to under one W/m2 for
the current net climate forcing [3].
(BTW, I think you are wrong about the OH. It is bacterial action by methanotrophs [4]
that oxidises the methane as it ascends through a water column. In
shallow seabed, such as ESAS where it is less than 50 metres deep, most of the
methane reaches the atmosphere without oxidation. As Stephen points out,
this methane digestion produces significant warming of the water column.)
So what can we reduce the risk of such a catastrophe? One absolutely requirement is to cool the Arctic using geoengineering and other means. As well as cooling the Arctic, we need to develop methods to capture (or flare) methane from the ocean seabed, preferably before (or as) it reaches the atmosphere.
The Arctic emergency situation, and measures to deal with it, will be
considered by the Arctic Methane Emergency Group (AMEG) at the conference organised by the Campaign against
Climate Change, in London,
on the weekend June 16-17th. Details are available
on the AMEG web site here [5]. All are welcome.
Cheers from Chiswick,
John
[1] http://www.realclimate.org/index.php/archives/2012/01/much-ado-about-methane/
[extract] Archer: "The methane bubbles coming from the Siberian shelf are
part of a system that takes centuries to respond to changes in temperature. The
methane from the Arctic lakes is also potentially part of a new, enhanced,
chronic methane release to the atmosphere. Neither of them could release a
catastrophic amount of methane (hundreds of Gtons) within a short time frame (a
few years or less). There isn’t some huge bubble of methane waiting to erupt as
soon as its roof melts."
[2] http://www.sciencemag.org/content/327/5970/1246.abstract
[3] http://www.columbia.edu/~jeh1/mailings/2011/20110415_EnergyImbalancePaper.pdf
[4] http://en.wikipedia.org/wiki/Methanotroph
[5] http://ameg.me/
Hi, all -
Going back to Stephen's suggestion, re arctic methane escape, elevated arctic CO2, and then the subsequent comments on OH, etc.: first, if there were a chronic release of CH4 to the arctic atmosphere, I don't think you would expect to see any elevated CO2 there at all, since the atmospheric mixing and CH4 lifetime are so different. On the other hand, the one case in which you would see this is that suggested by John Nissen's comment. I had written something once to AMEG suggesting there be a search for a small perturbation in CO2, as a test against just the same data he mentions from Shakhova et al. What John is discussing comes from sonar data, and if the observed seabed release rates were extrapolated over estimated ESAS taliks, it would give a few Gt/CH4 yr. But John then says that the water is too shallow there for much oxidation. Clearly those sonar readings, though, could only be meaningful if there were almost 100% oxidation of the methane in the water, since the growth in the atmosphere has been nothing on that scale. There is, surely, much about arctic microbial communities we don't know, so, just to speculate, if there really were such gigantic releases getting methanotrophically oxidized to CO2, how much of a CO2 anomaly might you expect to see locally? Crudely, if ~30Gt CO2 =+2ppm/yr, then you might expect that over ~3% of the atmosphere (arctic), 1 Gt/yr CO2 might equal ~2ppm. Microbes would be using some proportion of the carbon for biomass, but on the other hand 1Gt CH4 oxidizes >1Gt CO2, since the molecular weights are different, so if you imagine those factors roughly canceling each other out, then 1Gt methane oxidized in the water crudely gives ~1Gt CO2, and so you might expect a few Gt /yr could +~4-6ppm, which is about what you're seeing.
All that being said, given that these readings are all over the place, in Mongolia, Finland, Iceland, etc., I agree with Mike and transport is the easier explanation. At least let's hope so, because it would take an awful lot of methane, in other words, to make that small CO2 anomaly. One could test Stephen's suggestion, in any case, by looking locally at CO2 around hotspots of seabed release.
In terms of what Robert Socolow asks, which one also needs to know, I remember reading some years ago speculation on whether the annual (globally averaged) Mona Loa oscillation might be growing, perhaps as a signature of the fertilization effect. Could the arctic amplitude be increasing in this way, from things like the "pop up forests" that I just saw mentioned in the news yesterday, where tundra is rapidly changing in response to warming?
Cheers,
Nathan
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