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From the June 2009 Special Editions | 23 comments

The Arctic Thaw Could Make Global Warming Worse ( Preview )

The melting Arctic is releasing vast quantities of methane. How big is this greenhouse threat? What can be done?

By Sarah Simpson   

 

Methane is emitted anywhere organic matter ferments—be that a cow’s belly or frozen soil that starts to thaw. Permafrost, which averages 80 feet thick, is chock-full of dead plant and animal matter that has been locked in cold storage for thousands of years. Conventional wisdom long held that permafrost should take thousands of years to melt away, so researchers expected it to play a negligible role in climate change. But recent findings—Walter’s lake discovery in particular—have wrecked that prediction.

Walter’s work revealed that the relatively warm lake bed was indeed thawing the frozen earth directly below it, down several dozen feet. Thawing a block of permafrost is like taking a package of frozen hamburger out of the freezer and leaving it on the kitchen counter. As the meat warms, ravenous microbes consume it, giving off a gas as a by-product. On dry land, microbes convert the dead animal and plant matter primarily into CO2. But in the wet, oxygen-starved depths of a lake, they instead release methane. Walter’s best guess is that researchers have been underestimating methane emissions from Arctic wetlands by as much as 63 percent.

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