The first one repeats what has already been shown — that there is a long - term process of slow destabilization of
seabed methane.
Offshore permafrost decay and massive
seabed methane escape in water depths > 20 m at the South Kara Sea shelf
The research vessel Helmer Hanssen spent 3 - weeks on an expedition to
seabed methane seeps in the Arctic Ocean around Svalbard.
Thawing by climate change of subsea layer of permafrost may release stores of underlying,
seabed methane
-- Increasing release of carbon stored in soils and permafrost and methane from
seabed methane hydrates
Despite portentous headlines — including one on the news release from the University of Alaska, Fairbanks, saying «Arctic
seabed methane stores destabilizing...» — there is no evidence (yet) that what is happening is fundamentally new or destabilizing, at least according to some of the scientists most closely tracking levels and sources of this gas from the poles to the tropics.
In case you missed it, there's more on
the seabed methane emissions from Justin Gillis on the Green blog and an analysis of methane media coverage by Charles Petit at the Knight Science Journalism Tracker and another by Curtis Brainard at the Columbia Journalism Review.
The Arctic
seabed methane rate of release, on the other hand, is likely to increase, as you point out.
I just go to the section where they get into discussing Arctic
seabed methane in more detail, and the conclusion of that section is actually: «In summary, the ocean methane hydrate pool has strong potential to amplify the human CO2 release from fossil fuel combustion over time scales of decades to centuries.»
How fast that warming could affect the release of
seabed methane?
Not exact matches
A recent study in Geochemistry, Geophysics and Geosystems strongly links
methane leaks from the
seabed off Western Svalbard with tremors of the Earth.
A major release of
methane trapped in the frozen
seabed off Russia could accelerate global warming and cause $ 60 trillion in damage, almost the size of world GDP, it said.
The United States has released an ambitious, climate - and conservation - focused agenda for its 2 - year chairmanship that includes pushing for more research on black carbon, which accelerates melting in the region, and on emissions of the potent greenhouse gas
methane from the
seabed and permafrost, as well as creating a network of marine protected areas in the Arctic and equipping Arctic villages with renewable energy sources.
• Our claim that 500 tonnes of
methane per square kilometre was bubbling up from the Arctic
seabed (30 November, p 18) was inflated: it should have read 500 kilograms.
Their analysis, published this week in Marine and Petroleum Geology, revealed that the structures are likely a result of their location: directly above a subsurface fault still hidden by the
seabed, where
methane oozes out of Earth's crust in various ways.
The study observed active
methane plumes rising from the
seabed, but most of the gas was not from hydrates and much of it did not reach the atmosphere.
A new study in Geochemistry, Geophysics and Geosystems strongly links
methane leaks from the
seabed off Western Svalbard with tremors of the Earth.
Measurements from the
seabed, the air and from land stations, along with modelling analysis, will provide the link between potential sources of elevated
methane concentrations and the reason for variations.
Methane gas released from the seabed during the summer months leads to an increased methane concentration in the
Methane gas released from the
seabed during the summer months leads to an increased
methane concentration in the
methane concentration in the ocean.
It occurs in
seabed layers at sites (such as the Barents Sea) that are rich in
methane.
As domes of frozen
methane destabilized within this
seabed some 12,000 years ago, they blasted open the seafloor.
Methane clathrate has accumulated below the
seabed over millions of years.
This 15 - metre - deep salt lake is caused by
methane, given off by rotting matter on the
seabed.
Underwater permafrost acts as a lid to restrain
methane stored in the
seabed.
Recent
methane measurements at Terceira Island, Azores, Portugal and Tae - ahn Peninsula, Republic of Korea (See http://www.esrl.noaa.gov/gmd/dv/iadv/index.php) in the context of outlier data points over the last decade at sites such as Storhofdi, Vestmannaeyjar, Iceland, and reports of
methane releases from the Arctic
seabed, tell us that at current levels of AGW, the Earth's sea - floor
methane systems are not stable.
Studies from 55 million years ago show possibility of eruption of
methane from the
seabed with enormous self - sustained warming.
If you look at the evidence (as opposed to models) of
methane from the Arctic
seabed, as collected by Shakhova and Semiletov, then you have to treat the possibility of
methane escalation extremely seriously.
What about just encouraging some of the beasties that already thrive in high
methane and low oxygen to propagate on the
seabed?
Studies from 55 million years ago (PETM excursion) show a possiblity that the eruption of
methane from the
seabed could intensify enormous self - sustained warming.
The concern, as I understand it, is that pathways in the latter areas can bring undissolved
methane up to the
seabed surface, and from there it can make it way through the shallow water column into the ocean surface.
Updated, 12:47 p.m. On another Arctic front, the notion that a huge outburst of heat - trapping
methane is nigh from the
seabed off Siberia, here's an update:
«This expedition was organized on a short notice by the Russian Fund of Fundamental Research and the U.S. National Science Foundation following the discovery of a dramatic increase in the leakage of
methane gas from the
seabed in the eastern part of the Arctic», said Professor Igor Semiletov, the head of the expedition.
You know what?I still firmly believe that the Earth will stabilise at 1000ppm by the year 2150, and I firmly believe that
methane outgassing from both the Arctic
seabed and frozen terrestial permafrost will have a huge impact on this number, helping it to rise to 1000 ppm by the year 2150.
Fresh headlines followed publication of «Ebullition and storm - induced
methane release from the East Siberian Arctic Shelf,» a new Nature Geoscience paper from Natalia Shakhova, Igor Semiletov and the rest of a team tracking emissions of this important greenhouse gas from the
seabed and shallow waters off Siberia.
Dec. 29, 9:28 a.m. Updated below I've been in touch with Natalia Shakhova and Igor Semiletov, the intrepid Russian researchers, based at the International Arctic Research Center in Fairbanks, Alaska, who for more than a decade have been leading an important international project analyzing
methane plumes rising from the
seabed in the shallow Arctic waters spreading north from eastern Siberian shores.
Apparently, Arctic storms increase
methane release from the
seabed.
New data obtained in our 2011 cruise and other unpublished data give us a clue to reevaluate if the scale of
methane releases from the East Siberian Arctic Shelf
seabed is assessed correctly (papers are now in preparation).
(There is also the argument from the practical: I suspect that if you could put a straw into the
seabed and suck out enough free
methane to change the world, the oil companies would have figured it out by now...)
«An ice - free Arctic could be this year, in September,» McPherson says, «and this could lead to a burst of
methane at any time» from the shallow Arctic
seabed.
Tagsmethane,
Methane Emissions, Arctic
Seabed, Arctic, Greenhouse gas, greenhouse gas emissions, carbon dioxide, climate change, natural gas
Scientists estimate that there are hundreds of millions of tonnes of
methane gas locked away beneath the Arctic permafrost, which extends from the mainland into the
seabed of the relatively shallow sea of the East Siberian Arctic Shelf.
Methane can also be stored in the seabed as methane gas or methane hydrates and then released as subsea permafrost
Methane can also be stored in the
seabed as
methane gas or methane hydrates and then released as subsea permafrost
methane gas or
methane hydrates and then released as subsea permafrost
methane hydrates and then released as subsea permafrost thaws.
Large amounts of
methane are produced in anaerobic conditions by bacterial activity in the sediments below the
seabed as well as by chemical transformation of organic matter at greater burial depths.
An even more worrying potential source of greenhouse gases is the
methane in the
seabed of the Arctic Ocean, notably off the coast of Siberia.
Methane hydrate in ocean seabed sediments is a potential source of methane (CH4) to the atmosphere, where CH4 has potential to act as a powerful greenhou
Methane hydrate in ocean
seabed sediments is a potential source of
methane (CH4) to the atmosphere, where CH4 has potential to act as a powerful greenhou
methane (CH4) to the atmosphere, where CH4 has potential to act as a powerful greenhouse gas.
First, given that Arctic
seabeds are now releasing
methane from gas hydrates at present levels of global warming, the 2 ° limit and carbon budget that Paul refers to is simply irrelevant.
Measurements from the
seabed, the air and from land stations, along with modelling analysis, will provide the link between potential sources of elevated
methane concentrations and the reason for variations.
It is also worth noting that the use of both modes of Geo - E in a Troika strategy can not entirely guarantee a benign outcome, however long the R&D period, since we have no firm information on how large the response the
Methane Hydrates Melt feedback will be to the sum of ocean warming that is already penetrating the
seabed plus that from the several decades of further warming as the natural sea temperatures are slowly restored.
This summer, scientists taking part in the six - week International Siberian Shelf Study discovered numerous areas, spread over thousands of square miles, where large quantities of
methane — a gas with 20 - times the heat - trapping power of carbon dioxide — rose from the once - frozen
seabed floor.
«Previous observations have pointed to large
methane plumes being released from the
seabed in the relatively shallow sea off the northern coast of Siberia, but the latest findings were made far away from land in the deep, open ocean where the surface is usually capped by ice.»