Friday on my mind (once more)

coccolith.jpg Before you ask, the picture shows the shell of a coccolithophore, and it’s in trouble. We’ve been adding a lot of carbon dioxide to the atmosphere, and a good chunk of it has ended up in the oceans. The water is getting more acidic, and some sea creatures are finding it harder to build their shells – which has the potential to disrupt the entire oceanic food web. We know it’s a problem, we know it’s happening, but we didn’t expect it be happening as fast as a recent research programme has found [Herald, Telegraph]. According to one of the scientists involved, “the coastal ocean acidification train has left the station, and there’s not much we can do to derail it.” Another excellent reason to cut carbon emissions, if one was needed.

More on methane: research on a rapid release of methane hydrates 635 million years ago hints that modern warming could trigger a similar cascade of gas release, with catastrophic results for the planet’s climate [Science Daily News, Wired]. Wired also has an excellent backgrounder on methane hydrates, discussing how they might be turned into a source of energy, while the BBC reports that the recent rise in methane in the atmosphere looks as though it is coming from thawing wetlands in the Arctic. In better news, NZ scientists have completed deciphering the genome of one of the methanogens that live in the rumens of cattle and sheep (Stuff, Yahoo/xtra). With luck and a lot of hard work, this might lead to methods of cutting methane emissions from livestock, and eventually play a key role in reducing agricultural emissions around the world.

Some light reading for the weekend: Yale’s environment360 is a new web site from the Yale School of Forestry & Environmental Studies, launched this month with some interesting and challenging articles from writers like Elizabeth Kolbert, Bill McKibben, and Fred Pearce amongst others. Worth checking out.

For those with more than a few minutes to spare, I can recommend The Economics of Ecosystems and Biodiversity review [PDF] released this week. It’s an attempt to put a rational value on the services nature provides, to allow a Stern Review-type of cost benefit analysis of losing or retaining biodiversity [Herald, BBC, Guardian]. Climate change is only one contributor to biodiversity loss, but it could rapidly become the most important, and it’s the world’s poor that will suffer most.

It’s a gas, gas, gas

arcticmethane.jpg It’s not good news. The USA’s National Oceanic and Atmospheric Administration (NOAA) has produced its annual report on greenhouse gas levels in the atmosphere, and carbon dioxide concentration continues its accelerated growth. And there are signs that methane levels are beginning to rise, after a decade of remaining more or less static. The BBC reports:

NOAA figures show CO2 concentrations rising by 2.4 parts per million (ppm) from 2006 to 2007. By comparison, the average annual increase between 1979 and 2007 was 1.65ppm.

The methane rise is worrying because it’s a very powerful greenhouse gas (23 times as effective at trapping heat as CO2), and there are a number of positive feedbacks that could come into play as the planet warms. From the NOAA release:

Rapidly growing industrialization in Asia and rising wetland emissions in the Arctic and tropics are the most likely causes of the recent methane increase, said scientist Ed Dlugokencky from NOAA’s Earth System Research Laboratory. ”We’re on the lookout for the first sign of a methane release from thawing Arctic permafrost,” said Dlugokencky. “It’s too soon to tell whether last year’s spike in emissions includes the start of such a trend.”

Permafrost is one thing, methane hydrates are another. Sometimes called burning ice, methane hydrates (aka clathrates) are a mixture of ice and methane that exist in large quantities on the sea floor – and there are particularly large amounts in the shallow Arctic seas north of Russia and Siberia (more info at Climate Progress). At the recent European Geophysical Union conference in Vienna, a Russian scientist discussed the issue. From SpiegelOnline:

In the permafrost bottom of the 200-meter-deep sea [off the northern coast of Siberia], enormous stores of gas hydrates lie dormant in mighty frozen layers of sediment. The carbon content of the ice-and-methane mixture here is estimated at 540 billion tons. “This submarine hydrate was considered stable until now,” says the Russian biogeochemist Natalia Shakhova, currently a guest scientist at the University of Alaska in Fairbanks who is also a member of the Pacific Institute of Geography at the Russian Academy of Sciences in Vladivostok.

The permafrost has grown porous, says Shakhova, and already the shelf sea has become “a source of methane passing into the atmosphere.” The Russian scientists have estimated what might happen when this Siberian permafrost-seal thaws completely and all the stored gas escapes. They believe the methane content of the planet’s atmosphere would increase twelvefold. “The result would be catastrophic global warming,” say the scientists.

The SpeigeOnline article is worth reading in full. Shakova’s observations of methane emissions hint at an explanation for the increase in global atmospheric methane. If that’s the case – and its too early to say for sure – then we may be seeing the beginnings of one of the most worrying of the positive carbon cycle feedbacks – one that could potentially make anything we do to cut CO2 emissions the equivalent of pissing in the wind.

[Hat tip for the Spiegel piece to No Right Turn – I’m frankly amazed the EGU paper hasn’t had much more coverage in the world’s media.]

[Update for the interested: The EGU abstract for Shakhova’s paper is here [PDF]. Here’s the last few words:

“…we consider release of up to 50 Gt of predicted amount of hydrate storage as highly possible for abrupt release at any time. That may cause ~ 12-times increase of modern atmospheric methane burden with consequent catastrophic greenhouse warming.”

“Abrupt release at any time”. That’s truly alarming.]

Here come the warm jets

Hot Topic has devoted a lot of posts to events in the Arctic over the last northern hemisphere summer. The loss of sea ice was dramatic – there was 25% less ice in September than the previous record, set in 2005. The little graph to the left shows just far off the trend line last year’s September area really was. And as I posted yesterday, recent studies suggest that the Arctic is primed for more significant losses in the near future. If the reduction in summer sea ice continues, there are some pretty major implications for the climate of the northern hemisphere and for our modelling of the global climate, and it’s those things that I want to consider in this post. Please note: I am not a climate scientist, and there are a lot of ifs and handwaves in this argument, but bear with me…

Continue reading “Here come the warm jets”

Something 4 The Weekend

Bali continues to make headlines. The rough positions are becoming clear. China’s playing hardball – no mandatory cuts, West has to cut first and most deeply. The New York Times‘ Andy Revkin has a couple of good Bali posts on his blog: the first suggests that the IPCC may have to revise its goal for the next report – updating AR4 for the conclusion of the post-Kyoto process in 2009, while the second looks at what’s going on around the negotiations. Meanwhile, 200 scientists from around the world, coordinated by the Climate Change Research Centre at the University of New South Wales, issued a statement calling on the conference to aim for emissions cuts of at least 50% by 2050 [Herald, Globe & Mail (Canada)].

Meanwhile, there’s lots more below the fold (as they say on the broadsheets)….

Continue reading “Something 4 The Weekend”

Formerly the weekend roundup

Saturday’s promised omnibus extension never arrived, in part because of the arrival of a big cat on my computer, so here’s a Tuesday update.

Continue reading “Formerly the weekend roundup”