Climate-changing
methane 'rapidly destabilizing' off East Coast, study finds
24
October, 2012
A
changing Gulf Stream off the East Coast has destabilized frozen
methane deposits trapped under nearly 4,000 square miles of seafloor,
scientists reported Wednesday. And since methane is even more potent
than carbon dioxide as a global warming gas, the researchers said,
any large-scale release could have significant climate impacts.
Temperature
changes in the Gulf Stream are "rapidly destabilizing methane
hydrate along a broad swathe of the North American margin," the
experts said in
a study published Wednesday in the peer-reviewed journal Nature.
Using
seismic records and ocean models, the team estimated that 2.5
gigatonnes of frozen methane hydrate are being destabilized and could
separate into methane gas and water. It is not clear if that is
happening yet, but that methane gas would have the potential to rise
up through the ocean and into the atmosphere, where it would add to
the greenhouse gases warming Earth.
The
2.5 gigatonnes isn't enough to trigger a sudden climate shift, but
the team worries that other areas around the globe might be seeing a
similar destabilization.
"It
is unlikely that the western North Atlantic margin is the only area
experiencing changing ocean currents," they noted. "Our
estimate ... may therefore represent only a fraction of the methane
hydrate currently destabilizing globally."
The
wider destabilization evidence, co-author Ben Phrampus told NBC News,
includes data from the Arctic and Alaska's northern slope in the
Beaufort Sea.
And
it's not just under the seafloor that methane has been locked up.
Some Arctic land area are seeing permafrost thaw, which could release
methane stored there as well.
An
expert who was not part of the study said it suggests that methane
could become a bigger climate factor than carbon dioxide.
"We
may approach a turning point" from a warming driven by man-made
carbon dioxide to a warming driven by methane, Jurgen Mienert, the
geology department chair at Norway's University of Tromso, told NBC
News.
"The
interactions between the warming Arctic Ocean and the potentially
huge methane-ice reservoirs beneath the Arctic Ocean floor point
towards increasing instability," he added
He
also noted, however, that "one of the big unknowns is the
magnitude of rapid methane escape from the ocean floor, and how
natural filter systems react and affect the future ocean, its
environment and the climate."
Another
unknown is what caused the Gulf Stream changes, said Phrampus, an
earth sciences PhD candidate at Southern Methodist University in
Dallas, Texas.
"Multiple
events can play a factor, such as changing sea level or an addition
of cold/fresh water from the north," Phrampus said, adding he
was hopeful that the changes might be "reversible under
their own influence."
But,
he added, "we need more data to resolve this, and we are
currently investigating this process."
For
thousands of years, permafrost has trapped Siberia's carbon-rich
soil, a compost of Ice Age plant and animal remains. But global
warming is melting the permafrost and exposing the soil, causing
highly flammable methane to seep out. NBC's Jim Maceda reports.
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