flacaltenn
Diamond Member
- Jun 9, 2011
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The release of methane from the Arctic is in itself a contributor to global warming as a result of polar amplification. Recent observations in the Siberian arctic show increased rates of methane release from the Arctic seabed.[4] Land-based permafrost, also in the Siberian arctic, was also recently observed to be releasing large amounts of methane, estimated at over 4 million tons – significantly above previous estimates.[11]
In the plot showing the global atmospheric methane concentration (the significant measure from the viewpoint of global warming and radiative forcing), however, the rate of the increase in atmospheric methane has been slowing until 2004, indicating that the contribution from Arctic release is currently not the dominant factor in the global picture.
Current methane release has previously been estimated at 0.5 Mt per year.[12] Shakhova et al. (2008) estimate that not less than 1,400 Gt of Carbon is presently locked up as methane and methane hydrates under the Arctic submarine permafrost, and 5-10% of that area is subject to puncturing by open taliks. They conclude that "release of up to 50 Gt of predicted amount of hydrate storage [is] highly possible for abrupt release at any time". That would increase the methane content of the planet's atmosphere by a factor of twelve.[13]
In 2008 the United States Department of Energy National Laboratory system[14] identified potential clathrate destabilization in the Arctic as one the most serious scenarios for abrupt climate change, which have been singled out for priority research. The U.S. Climate Change Science Program released a report in late December 2008 estimating the gravity of the risk of clathrate destabilization, alongside three other credible abrupt climate change scenarios.[15]
4. ^ a b c Shakhova, Natalia (2005). "The distribution of methane on the Siberian Arctic shelves: Implications for the marine methane cycle". Geophysical Research Letters 32 (9): L09601. Bibcode:2005GeoRL..3209601S. doi:10.1029/2005GL022751.
11. ^ Walter, Km; Zimov, Sa; Chanton, Jp; Verbyla, D; Chapin, Fs, 3Rd (Sep 2006). "Methane bubbling from Siberian thaw lakes as a positive feedback to climate warming". Nature 443 (7107): 71–5. Bibcode:2006Natur.443...71W. doi:10.1038/nature05040. ISSN 0028-0836. PMID 16957728.
12. ^ Shakhova N., Semiletov I., Salyuk A., Kosmach D., Bel'cheva N. (2007). "Methane release on the Arctic East Siberian shelf". Geophysical Research Abstracts 9: 01071.
13. ^ N. Shakhova, I. Semiletov, A. Salyuk, D. Kosmach (2008), Anomalies of methane in the atmosphere over the East Siberian shelf: Is there any sign of methane leakage from shallow shelf hydrates?, EGU General Assembly 2008, Geophysical Research Abstracts, 10, EGU2008-A-01526
14. ^ IMPACTS: On the Threshold of Abrupt Climate Changes, Lawrence Berkeley National Laboratory News Center, 17 September 2008
15. ^ CCSP, 2008: Abrupt Climate Change. A report by the U.S. Climate Change Science Program and the Subcommittee on Global Change Research (Clark, P.U., A.J. Weaver (coordinating lead authors), E. Brook, E.R. Cook, T.L. Delworth, and K. Steffen (chapter lead authors)). U.S. Geological Survey, Reston, VA, 459 pp.
That's REALLY interesting.. Because I was cruising thru this list of cites JUST LAST NIGHT and read the actual abstract from Shakova (2008).. It's here below..
Which paper was the quote from? Because they left out a KEY PIECE OF INFORMATION..
http://www.cosis.net/abstracts/EGU2008/01526/EGU2008-A-01526.pdf\
Anomalies of methane in the atmosphere over the East
Siberian shelf: Is there any sign of methane leakage
from shallow shelf hydrates?
N. Shakhova (1,2), I. Semiletov (1,2), A. Salyuk (2), D. Kosmach (2)
(1) International Arctic Research Center of the University of Alaska Fairbanks, USA
([email protected]) (2) V.I. Il’ichov Pacific Oceanological Institute, Far-eastern Branch
of Russian Academy of Sciences, Vladivostok, Russia
Methane release from continental margins is widespread and contributes methane to
the biosphere, hydrosphere, and atmosphere, thus making up an important part of
the global carbon cycle. The contribution of arctic shallow seabed sediments to the
global carbon budget and, particularly, to the marine methane budget, has received
little attention because the area of these sediments is small in extent and because,
due to low temperatures that characterize these sediments, they are not considered
conducive to methanogenesis. In addition, in the case of the East Siberian Shelf (ESS),
shallow sediments have not been considered a methane source to the hydrosphere
or atmosphere because seabed permafrost (defined as sediments with a 2-year mean
temperature below 0°C), which is considered to underlay most of the ESS, acts as
an impermeable lid, preventing methane escape. However, our recent data showed
extreme methane supersaturation of surface water, implying high sea-to-air fluxes.
The total value of ESS carbon pool is, thus, not less than 1,400 Gt of carbon.
Since the area of geological disjunctives (fault zones, tectonically and seismically active areas) within the Siberian Arctic shelf composes not less than 1-2% of the total area and area of open taliks (area of melt through permafrost), acting as a pathway for methane escape within the Siberian Arctic shelf reaches up to 5-10% of the total area, we consider release of up to 50 Gt of predicted amount of hydrate storage as highly possible for abrupt release at any time. That may cause 12-times increase of modern atmospheric methane burden with consequent catastrophic greenhouse warming.
Ain't that cool? THIS is why I am a skeptic... Change the entire MEANING of a finding. Leave out a KEY assertion.. You are supporting dishonest science.. You just demonstrated it in action...
Once you give us the cite for that particular abstract -- us skeptics will thank you for contributing to our cause..
Nothing personal -- you are just too trusting...
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