Greenhouse gas leaking from Arctic Ocean floor
Noreen Parks
Environ. Sci. Technol., Article ASAP
DOI: 10.1021/es9026387
Publication Date (Web): September 16, 2009
Copyright © 2009 American Chemical Society
Scientists have
http://www.agu.org/pubs/crossref/2009/2009GL039191.shtml">reported the presence of previously unknown sources of methane—a greenhouse gas some 25 times more powerful than CO
2 at trapping heat—bubbling up from the Arctic Ocean seafloor north of Norway. Gradual warming of a regional current has caused temperature-sensitive methane hydrate below the seabed to break down and discharge the gas, the researchers say.
For years, scientists have debated whether the planet’s rising temperatures would turn methane deposits in permafrost regions into a “ticking bomb” that, once detonated, could liberate vast quantities of methane to the atmosphere, possibly triggering disastrous climate-feedback effects. Some paleoclimate studies have argued that such scenarios have occurred in the past, and that the processes of hydrate formation and disintegration have been a primary driver of glacial cycles.
Over the past couple of decades, as the tools for oceanographic exploration have grown more sophisticated, researchers have documented about 90 oceanic locations of
http://en.wikipedia.org/wiki/Methane_hydrate">methane hydrate, estimated to contain as much as 63,000 gigatons or more of carbon. Previously, International Polar Year (2007) surveys of the East Siberian Arctic shelf
http://www.iarc.uaf.edu/highlights/2008/ISSS-08/">uncovered abundant methane seeps and measured record-breaking summertime concentrations of the gas in northern polar waters.
Hydrate usually forms in sediment beneath the seabed and is stable at depths below 300−500 meters (m), depending upon temperature, pressure, salinity, and the types of gases present, according to Graham Westbrook of the University of Birmingham (U.K.). However, on a research cruise in 2008, Westbrook and colleagues collected sonar images of more than 250 plumes of methane gas rising from the seafloor at depths ranging between 150 and 400 m. They found these plumes along a section of continental margin washed by the West Spitsbergen Current (WSC), an arm of the Gulf Stream that delivers Atlantic seawater to the Arctic. As the WSC has warmed by 1 °C over the past 30 years, the depth at which hydrate in the area is stable has fallen from 360 to 396 m, liberating methane, Westbrook says.
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