Furthermore, the data reveal that the methane - derived carbon was mixed from the surface ocean downward, suggesting that a significant fraction of the initial dissociated hydrate
methane reached the atmosphere prior to oxidation.
Not exact matches
WHEN Stanley Miller and Harold Urey created amino acids by shooting sparks through a «primordial
atmosphere» of
methane, ammonia, hydrogen and water, biologists thought a full understanding of the origins of life was within
reach.
It remains to be seen whether such abrupt and massive
methane release could have
reached the
atmosphere.
But so far, as Dickens says, no one has shown that quantities of
methane large enough to change the climate would
reach the
atmosphere.
In deeper parts of the ocean, the
methane released from the ocean floor would likely never make it up to the
atmosphere, since it would get used up by microbes before it
reached the surface.
Exponentially less
methane would be able to
reach the
atmosphere in waters that are thousands of feet deep at the very edge of the shallow seas near continents, which is the area of the ocean where the bulk of
methane hydrates are,» Sparrow says.
Although the researchers did not examine in this study what prevents
methane released from the seafloor from
reaching the
atmosphere, they suspect it is biodegraded by microorganisms in the ocean before it hits the surface waters.
«No one has yet shown that CH4 [
methane] from hydrates is
reaching the
atmosphere today,» Thornton says.
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.
Most
methane hydrates are buried in ocean water so deep that the journey through the water column is too far for the gas to ever
reach the
atmosphere, according to Ed Dlugokencky, a researcher at the National Oceanic and Atmospheric Administration.
(
Methane forms as a by - product of anaerobic bacterial decomposition of organic matter in the soil and
reaches the
atmosphere through the roots and stems of the rice plants.)
Methane breakdown is a globally important process because «it keeps massive quantities of methane — a potent greenhouse gas — from reaching the overlying waters and atmosphere,» says microbiologist David Valentine of the Scripps Institution of Oceanography in La Jolla, Cali
Methane breakdown is a globally important process because «it keeps massive quantities of
methane — a potent greenhouse gas — from reaching the overlying waters and atmosphere,» says microbiologist David Valentine of the Scripps Institution of Oceanography in La Jolla, Cali
methane — a potent greenhouse gas — from
reaching the overlying waters and
atmosphere,» says microbiologist David Valentine of the Scripps Institution of Oceanography in La Jolla, California.
The ExoMars Trace Gas Orbiter, a Russian - launched, European - built spacecraft that arrived at Mars in October, is starting to dip into the upper
reaches of the red planet's
atmosphere in a year - long «aerobraking» campaign place the observatory in the right position to hunt for
methane, an indicator of potential biological activity.
Near - infrared observations have detected small clouds of
methane gas forming and dissipating in the upper
reaches of Titan's
atmosphere.
I believe that reaction takes much longer than bubbles require to
reach the surface; the
methane released in these bubble sites or in rapid events like underwater landslides) either dissolves in water or
reaches the
atmosphere in a matter of minutes, according to what was posted here earlier.
Two recent studies of
methane emissions from frozen sea - bed sediments, including one published in Science and described in The Times today, found substantial bubbling flows of
methane, a potent greenhouse gas, were
reaching the
atmosphere.
However, most of the
methane is virtually certain to remain trapped underground and will not
reach the
atmosphere.
Scientists are somewhat concerned that this leaking
methane may eventually
reach the
atmosphere, contributing to climate change, but only time will tell.
Most of the
Methane is NOT
Reaching the
Atmosphere, YET.
Reaching 400 ppm CO2 in the
atmosphere is inching ever closer to the tipping point when
methane takes over and kicks global warming into high gear.
Scientists have found that ancient reservoirs of
methane do not
reach the
atmosphere due to a role played by ocean waters.
While glaciers and ice sheets may physically plug large stores of buried
methane hydrates or pull carbon dioxide out of the
atmosphere through millions of small holes, their impacts
reach much further than their physical footprint.
In a new study, researchers claimed that a group of
methane - munching microbes that live in rocky dwellings on the seafloor could be preventing large amounts of greenhouse gas from
reaching the surface of the ocean and the
atmosphere, where it could contribute to rising global temperatures.
Most of the
methane gas that emerges from the sea floor dissolves in the water column and oxidizes to CO2 instead of
reaching the
atmosphere.
Methane hydrate floats in seawater just as water ice floats, and it also has greater potential to reach the atmosphere than methane bubbles (Brewer et al.,
Methane hydrate floats in seawater just as water ice floats, and it also has greater potential to
reach the
atmosphere than
methane bubbles (Brewer et al.,
methane bubbles (Brewer et al., 2002).
One is that seafloor
methane is apparently not
reaching the sea surface, and so is not
reaching the
atmosphere.
Essentially,
methane from decomposing garbage is captured and burned, preventing it from
reaching the
atmosphere.
RealClimate is wonderful, and an excellent source of reliable information.As I've said before,
methane is an extremely dangerous component to global warming.Comment # 20 is correct.There is a sharp melting point to frozen
methane.A huge increase in the release of
methane could happen within the next 50 years.At what point in the Earth's temperature rise and the rise of co2 would a huge
methane melt occur?No one has answered that definitive issue.If I ask you all at what point would huge amounts of extra
methane start melting, i.e at what temperature rise of the ocean near the Artic
methane ice deposits would the
methane melt, or at what point in the rise of co2 concentrations in the
atmosphere would the
methane melt, I believe that no one could currently tell me the actual answer as to where the sharp melting point exists.Of course, once that tipping point has been
reached, and billions of tons of
methane outgass from what had been locked stores of
methane, locked away for an eternity, it is exactly the same as the burning of stored fossil fuels which have been stored for an eternity as well.And even though
methane does not have as long a life as co2, while it is around in the air it can cause other tipping points, i.e. permafrost melting, to arrive much sooner.I will reiterate what I've said before on this and other sites.
Methane is a hugely underreported, underestimated risk.How about RealClimate attempts to model exactly what would happen to other tipping points, such as the melting permafrost, if indeed a huge increase in the melting of the methal hydrate ice WERE to occur within the next 50 years.My amateur guess is that the huge, albeit temporary, increase in
methane over even three or four decades might push other relevent tipping points to arrive much, much, sooner than they normally would, thereby vastly incresing negative feedback mechanisms.We KNOW that quick, huge, changes occured in the Earth's climate in the past.See other relevent posts in the past from Realclimate.Climate often does not change slowly, but undergoes huge, quick, changes periodically, due to negative feedbacks accumulating, and tipping the climate to a quick change.Why should the danger from huge potential
methane releases be vievwed with any less trepidation?
New research, some of it involving Howarth but led by chemists at Purdue University, seems to show that drills can open up gas pockets even before they
reach their target in the shale, and that this can send big plumes of
methane into the
atmosphere.
And even if that happened, many scientists say that the
methane released would largely be consumed in the sea (by bacteria that specialize in eating
methane) and would not
reach the
atmosphere.
Concentrations of dissolved
methane on the Siberian shelf
reached 25 times higher than atmospheric saturation, indicating escape of
methane from coastal erosion into the
atmosphere [Shakhova et al., 2005].