Scientists
have identified thousands of sites in the Arctic where methane that has been
stored for many millennia is bubbling into the atmosphere. The
methane has been trapped by ice, but is able to escape as the ice melts. Writing
in the journal Nature Geoscience, the researchers say this ancient gas could
have a significant impact on climate change. Methane is the second most
important greenhouse gas after CO2 and levels are rising after a few years of
stability. There are many sources of the gas around the world, some natural and
some man-made, such as landfill waste disposal sites and farm animals. Tracking
methane to these various sources is not easy.
But the researchers on the new
Arctic project, led by Katey Walter Anthony from the University of Alaska at
Fairbanks (UAF), were able to identify long-stored gas by the ratio of
different isotopes of carbon in the methane molecules. Using aerial and
ground-based surveys, the team identified about 150,000 methane seeps in Alaska
and Greenland in lakes along the margins of ice cover. Local sampling showed
that some of these are releasing the ancient methane, perhaps from natural gas
or coal deposits underneath the lakes, whereas others are emitting much younger
gas, presumably formed through decay of plant material in the lakes. "We
observed most of these cryosphere-cap seeps in lakes along the boundaries of
permafrost thaw and in moraines and fjords of retreating glaciers," they
write, emphasising the point that warming in the Arctic is releasing this
long-stored carbon.
If this relationship
holds true for other regions where sedimentary basins are at present capped by
permafrost, glaciers and ice sheets, such as northern West Siberia, rich in
natural gas and partially underlain by thin permafrost predicted to degrade
substantially by 2100, a very strong increase in methane carbon cycling will
result, with potential implications for climate warming feedbacks." Quantifying
methane release across the Arctic is an active area of research, with several
countries despatching missions to monitor sites on land and sea. The region
stores vast quantities of the gas in different places - in and under permafrost
on land, on and under the sea bed, and - as evidenced by the latest research -
in geological reservoirs. "The Arctic is the fastest warming region on the
planet, and has many methane sources that will increase as the temperature
rises," commented Prof Euan Nisbet from Royal Holloway, University of
London, who is also involved in Arctic methane research. "This is yet
another serious concern: the warming will feed the warming." How serious
and how immediate a threat this feedback mechanism presents is a controversial
area, with some scientists believing that the impacts will not be seen for many
decades, and others pointing out the possibility of a rapid release that could
swiftly accelerate global warming.
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