http://www.sciencedaily.com/releases/2011/11/111130215740.htm#.TthZQQuuESg.email

ScienceDaily (Nov. 30, 2011) — As global temperatures continue to rise at an 
accelerated rate due to deforestation and the burning of fossil fuels, natural 
stores of carbon in the Arctic are cause for serious concern, researchers say.

In an article scheduled to be published Dec. 1 in the journal Nature, a survey 
of 41 international experts led by University of Florida ecologist Edward 
Schuur shows models created to estimate global warming may have underestimated 
the magnitude of carbon emissions from permafrost over the next century. Its 
effect on climate change is projected to be 2.5 times greater than models 
predicted, partly because of the amount of methane released in permafrost, or 
frozen soil.
"We're talking about carbon that's in soil, just like in your garden where 
there's compost containing carbon slowly breaking down, but in permafrost it's 
almost stopped because the soil is frozen," Schuur said. "As that soil warms 
up, that carbon can be broken down by bacteria and fungi, and as they 
metabolize, they are releasing carbon and methane, greenhouse gases that cause 
warmer temperatures."

As a result of plant and animal remains decomposing for thousands of years, 
organic carbon in the permafrost zone is distributed across 11.7 million square 
miles of land, an amount that is more than three times larger than previously 
estimated. The new number is mainly based on evidence the carbon is stored much 
deeper as the result of observations, soil measurements and experiments.
"We know the models are not yet giving us the right answer -- it's going to 
take time and development to make those better, and that process is not 
finished yet," Schuur said. "It's an interesting exercise in watching how 
scientists, who are very cautious in their training, make hypotheses about what 
our future will look like. The numbers are significant, and they appear like 
they are plausible and they are large enough for significant concern, because 
if climate change goes 20 or 30 percent faster that we had predicted already, 
that's a pretty big boost."
The survey, which was completed following a National Science Foundation-funded 
Permafrost Carbon Network workshop about six months ago, proposed four warming 
scenarios until 2040, 2100 and 2300. Researchers were asked to predict the 
amount of permafrost likely to thaw, how much carbon would be released, and 
what amount would be methane, which has much more warming potential than carbon 
dioxide.
The occurrence of carbon in northern soils is natural and the chemical does not 
have an effect on climate if it remains underground, but when released as a 
greenhouse gas it can add to climate warming. However, humans could slow 
warming temperatures as the result of greenhouse gas emissions from 
deforestation and the burning of fossil fuels, which are what speed up the 
process of permafrost thaw.
"Even though we're talking about a place that is very far away and seems to be 
out of our control, we actually have influence over what happens based on the 
overall trajectory of warming. If we followed a lower trajectory of warming 
based on controlling emissions from the burning of fossil fuels, it has the 
effect of slowing the whole process down and keeping a lot more carbon in the 
ground," Schuur said. "Just by addressing the source of emissions that are from 
humans, we have this potential to just keep everything closer to its current 
state, frozen in permafrost, rather than going into the atmosphere."
The survey shows that by 2100, experts believe the amount of carbon released 
will be 1.7 to 5.2 times greater than previous models predict, under scenarios 
where Arctic temperatures rise 13.5 degrees Fahrenheit. Some predicted effects 
of global warming include sea level rise, loss of biodiversity as some 
organisms are unable to migrate as quickly as the climate shifts and more 
extreme weather events that could affect food supply and water resources.
"This new research shows that the unmanaged part of the biosphere has a major 
role in determining the future trajectory of climate change," said Stanford 
University biology professor Christopher Field, who was not involved in the 
study. "The implication is sobering. Whatever target we set for atmospheric 
CO2, this new research means we will need to work harder to reach it. But of 
course, limiting the amount of climate change also decreases the climate damage 
from permafrost melting."
When carbon is released from the ground as a result of thawing permafrost, 
there is no way of trapping the gases at the source, so action to slow its 
effect must be taken beforehand.
"If you think about fossil fuel and deforestation, those are things people are 
doing, so presumably if you had enough will, you could change your laws and 
adjust your society to slow some of that down," Schuur said. "But when carbon 
starts being emitted from the permafrost, you can't immediately say, 'OK, we've 
had enough of this, let's just stop doing it,' because it's a natural cycle 
emitting carbon whether you like it or not. Once we start pushing it, it's 
going to be releasing under its own dynamic."

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