This blog contains articles and commentary on Climate Change / Global Warming. These changes will have an affect on the entire planet and all of us who reside therein.
Life as we know it will change drastically. There is also the view that there is a high likelihood of climate change being a precursor of conflits triggered by resource shortges.
Friday, February 22, 2013
Major methane release is almost inevitable
We are on the cusp of a tipping point in the climate. If the global climate warms another few tenths of a degree, a large expanse of the Siberian permafrost will start to melt uncontrollably.
The result: a significant amount of extra greenhouse gases released into the atmosphere, and a threat – ironically – to the infrastructure that carries natural gas from Russia to Europe.
The Siberian permafrost is a particular danger. A large region called the Yedoma could undergo runaway decomposition once it starts to melt, because microbes in the soil would eat the carbon and produce heat, melting more soil and releasing ever more greenhouse gases. In short, the melting of Yedoma is a tipping point: once it starts, there may be no stopping it.
For the first time, we have an indication of when this could start happening.Anton Vaks of the University of Oxford in the UK and colleagues have reconstructed the history of the Siberian permafrost going back 500,000 years. We already know how global temperatures have risen and fallen as ice sheets have advanced and retreated, so Vaks's team's record of changing permafrost gives an indication of how sensitive it is to changing temperatures.
But there is no direct record of how the permafrost has changed, so Vaks had to find an indirect method. His team visited six caves that run along a south-north line, with the two southernmost ones being under the Gobi desert. Further north, three caves sit beneath a landscape of sporadic patches of permafrost, and the northernmost cave is right at the edge of Siberia's continuous permafrost zone.
The team focused on the 500,000-year history of stalagmites and similar rock formations in the caves. "Stalagmites only grow when water flows into caves," Vaks says. "It cannot happen when the soil is frozen." The team used radiometric dating to determine how old the stalagmites were. By building up a record of when they grew, Vaks could figure out when the ground above the caves was frozen and when it wasn't.
As expected, in most of the caves, stalagmites formed during every warm interglacial period as the patchy permafrost melted overhead.
But it took a particularly warm interglacial, from 424,000 and 374,000 years ago, for the stalagmites in the northernmost cave to grow – suggesting the continuous permafrost overhead melted just once in the last 500,000 years.
"Up until this point, we didn't have direct evidence of how this happened in past warming periods," says Ted Schuur of the University of Florida in Gainesville.
It will be very hard to stop the permafrost degrading as a warming of 1.5 °C is not far off. Between 1850 and 2005, global temperatures rose 0.8 °C,according to the 2007 report of the Intergovernmental Panel on Climate Change. Even if humanity stopped emitting greenhouse gases tomorrow, temperatures would rise another 0.2 °C over the next 20 years. That would leave a window of 0.5 °C – but in fact our emissions are increasing. What's more, new fossil fuel power stations commit us to several decades of emissions.
What are the consequences? The greatest concern, says Tim Lenton of the University of Exeter in the UK, is the regional landscape. Buildings and infrastructure are often built on hard permafrost, and will start subsiding. "Ice roads won't exist any more."
The increasingly soggy permafrost will also threaten the pipelines that transport Russian gas to Europe. "The maintenance and upkeep of that infrastructure is going to cost a lot more," says Schuur.
As for the methane that could be released into the atmosphere, Schuur estimates that emissions will be equivalent to between 160 and 290 billion tonnes of carbon dioxide. More