Wednesday, September 06, 2006

I blame James Nicoll

As the Earth warms, greenhouse gases once stuck in the long-frozen soil are bubbling into the atmosphere in much larger amounts than previously anticipated, according to a study in Thursday's journal Nature.

Methane trapped in a special type of permafrost is bubbling up at a rate five times faster than originally measured, the journal said.

Scientists are fretting about a global warming vicious cycle that had not been part of their already gloomy climate forecasts: Warming already under way thaws permafrost, soil that had been continuously frozen for thousands of years.

Thawed permafrost releases methane and carbon dioxide. Those gases reach the atmosphere and help trap heat on Earth in the greenhouse effect. The trapped heat thaws more permafrost, and so on.

"The higher the temperature gets, the more permafrost we melt, the more tendency it is to become a more vicious cycle," said Chris Field, director of global ecology at the Carnegie Institution of Washington. "That's the thing that is scary about this whole thing. There are lots of mechanisms that tend to be self-perpetuating and relatively few that tends to shut it off."

The effect reported in Nature is seen mostly in Siberia, but also elsewhere, in a type of carbon-rich permafrost, flash frozen about 40,000 years ago. A new more accurate measuring technique was used on the bubbling methane, which is 23 times more powerful a greenhouse gas than the more prevalent carbon dioxide.


I first heard about this via James Nicoll. That should have been a warning sign. James is noted for his harrowing tales of near death experiences that his family has had and yet still survives long enough to reproduce. I have no doubt now, that this is almost certainly going to be worse than even James thought it might be simply because James noted it first in my light cone. This means we're all screwed. Except James' gene line. 500 million years from now, his will be still around. Even if we have another PT level event or two.

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