Saturday, February 13, 2010

Climate science in the spotlight may not be such a bad thing

Climate science in the spotlight may not be a bad thing. Though as a climate scientist, the lights seem pretty bright and rather dazzling. I'm relieved they've not yet been on me. So what on earth possessed me to write this piece?

I get worried when I hear news presenters asking other news presenters whether these controversies should affect political efforts to achieve greenhouse gas emission reductions. Such a question demonstrates a misunderstanding of climate science, and of science more generally.

Perhaps people's perception of science originates from what they were taught at school. This "school science" is the source of solid facts and reliable understanding. Some of that science may be wrong, in the sense that it doesn't give the whole picture. Newton's laws of motion and gravity fit into that category; Einstein explained situations in which they fail. Yet even in such cases there is another sense in which they are right, or at least sufficiently accurate, because they help us understand and predict the particular thing we are studying. They are known to be "fit for purpose".

Such school science is very different to "research science". The former is about communicating what we already understand, the latter about developing and expanding our understanding. In research science new results and interpretations are continually developed. Disagreements and debate are common. Indeed they should be encouraged. And over time there is a shift of science from one to the other.

Climate change science is only unusual in this context because it has such huge significance for the world's societies. The public, the media, the politicians are all looking for answers from the science. Yet the understanding that drives the need for reducing greenhouse gas emissions has changed little over the past twenty years or so. I would argue that it has already moved from research science to school science.

It is rarely discussed by research scientists because it is so well understood. The chain of connections is a little too long to cover properly here. But fundamentally the properties of greenhouse gases means that increasing them traps more energy in the lower atmosphere. Putting more energy in warms things up. Even small changes in temperature have the potential to change the climate significantly; the last ice age may have been only five or six degrees colder than now when averaged across the globe. And of course global averages can hide large regional variations. Consequently we know we face increasing risks of everything from coastal inundation to changing water availability, changing ecosystems and knock–on effects to geopolitical stresses and security.

Maybe this sounds woolly. It is. There are still substantial uncertainties, even unknowns, regarding what will happen at any particular place and how it will affect the societies in which we live. These topics are still very much the domain of research. And believe me, the arguments among researchers about how to provide reliable predictions at local scales are lively and heated.

But such uncertainties are irrelevant to whether we need to reduce greenhouse gas emissions dramatically as soon as possible. There is no uncertainty that the consequences of climate change will be severe for global society, and therefore for us as members of that global society. The consequences for any individual may come through the direct effect of changes in local climate or it may come through changes to the working of, and stability of, global economic systems. Whatever the case, climate change represents a future of much increased risk. We would do well to act now to minimise those risks.

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Climate change: calling planet birth

Twelve years ago, the American author Bill ­McKibben published a short book entitled Maybe One: A Personal And Environmental Argument For Much Smaller Families. It certainly has its faults: most obviously, it provides a little too much information about the vasectomy ­McKibben decided to have in lieu of a second child. But it isn't pious or hectoring; if anything, the author tries overly hard to be tentative, emphasising that he isn't seeking to dictate other people's choices, and doesn't think he has all the answers. The "maybe" is right there in the title, after all. McKibben meant it in the sense of "maybe one child at most", but it reflects the book's general tone of modesty and equivocation. Maybe One is a suggestion. It's something to think about.

He might as well have called for the enforced sterilisation of all men and women of procreating age, along with the outlawing of Father Christmas and the Tooth Fairy. The New York Times called him "sanctimonious" and "holier-than-thou". The Wall Street Journal labelled him an "extremist" (their specific objection was that he hadn't mentioned nuclear power as a way to combat global warming, even though Maybe One is a book about parenting). "So much false information, so many bad ideas, in so few pages," another reviewer fumed. Speaking after publication, McKibben observed that Maybe One's subject matter was "the last remaining taboo thing to talk about" and in this case the cliché seemed justified.

In 1998, most people weren't willing to consider any significant lifestyle changes for environmental reasons, let alone cutting back on kids. Much has changed since then, of course, both in terms of the consensus on the threat posed by climate change, and our willingness to make sacrifices in the face of it. But one thing has not: you still won't hear any major environmental campaign group in Britain or the US arguing that, in addition to flying less and recycling more, middle-class westerners should be having fewer children to save the planet. Even commentators who warn of the evils of overpopulation, proudly trumpeting their willingness to raise controversial issues in defiance of "political correctness", only rarely emphasise the notion that we – rather than those in the developing world – might consider doing less of the populating. For several thorny reasons, family size has become the great unmentionable of the campaign for more environmentally friendly lifestyles. And yet, in the end, it may be the only one that really counts.

Trying to understand the debate about population and the climate sometimes feels like peering into a kaleidoscope while drunk. Directly contradictory claims, that can't both be true at the same time, are advanced as if they were facts. Weird allegiances are created: George Monbiot and American creationists, for example, are roughly equally contemptuous of organisations such as the Optimum Population Trust; supporters of reproductive rights find common cause with anti-abortionists. You come across nutty-sounding fringe groups like the Voluntary Human Extinction Movement, but then you phone its founder, Les Knight – he's a supply teacher, based on America's west coast, and can only talk during breaks between lessons – only to discover that he isn't nutty at all, but in fact rather sane and self-deprecating. (He simply wants people to choose not to breed. "Eventually we'll be extinct anyway, but it would be so much nicer if we phased ourselves out through natural attrition," Knight told me affably. "You know – the way a company reduces its workforce without firing anyone.")

For all the confusion and sensitivities that ­surround the subject, though, the basic facts are clear. If you live in Britain or the US in 2010, there is nothing you can do to reduce your impact on the environment that even comes close to the effects of having one fewer child.

This makes intuitive sense: every new human is a new consumer with their own carbon footprint, along with their own potentially limitless chain of descendants. The year before last, two researchers at Oregon State University, Paul Murtaugh and Michael Schlax, set about trying to put a figure on the idea of "carbon legacy", and last summer their results were published in the journal Global Environmental Change. Murtaugh and Schlax started from a simple premise. Assume, they said, that if a woman and a man have a baby, they're each responsible for 50% of that child's lifetime carbon dioxide emissions; and if that child has its own child, the original two parents each bear 25% of the responsibility for their grandchild's emissions, and so on down the generations. For how many tonnes, on average, would each original parent end up being responsible?

There are two important obstacles in performing this calculation. The first is that you don't know what will happen to per capita emission rates in the future: worldwide, they'll almost certainly rise, but in many ­western countries they're likely to fall, as energy-efficiency measures kick in. The second is that you don't know what will happen to fertility rates: you can't know whether your great-great-granddaughter will give birth to one new carbon-emitter, or two, or six, or zero. So for fertility rates, Murtaugh and Schlax used UN population predictions. (In the experiment, some of the hypothetical family trees eventually died out; others were stopped after a predetermined time.) And for per capita emissions, they used three different scenarios: an optimistic one, in which per capita emissions fell, a pessimistic one in which they rose, and a compromise one, in which they stayed constant.

The headline result was astonishing. Under the constant scenario, an American who forgoes having a child would save 9,441 tonnes of CO2 – almost six times, on average, the amount of CO2 they would emit in their own lifetime, or the equivalent of making around 2,550 return aero­plane trips between London and New York. If the same American drove a more fuel-efficient car, drastically reduced his or her driving, installed energy-efficient windows, used energy-efficient lightbulbs, replaced a household refrigerator, and recycled all household paper, glass and metal, he or she would save fewer than 500 tonnes.

The Oregon study didn't run the numbers for Britain, where per capita carbon emissions are already about half as big as in the US. (This isn't down to personal virtue: it's mainly because so many of our power stations use gas instead of coal.) But in every other country they examined – including Japan, where per capita emissions are similar to Britain's – the environmental effects of not having a child were similarly vast. Even if every emissions target recommended by the Intergovernmental Panel on Climate Change were to be successfully implemented – the ­"optimistic scenario" – an American could still save 562 tonnes of CO2 by having one fewer child, while a Japanese person could save 233 tonnes.

Leaving aside the complexities of global population issues, then, wouldn't it make sense for British environmental groups to suggest that well-off westerners might like to consider smaller families? John Sauven, the executive director of Greenpeace UK, concedes that it's a "no-brainer" that a smaller population would place a smaller burden on the planet. But he's reluctant to contemplate a Greenpeace campaign; in any case, he says, among environmentally conscious people in his demographic, "my sense is that nearly all of us have had two children or fewer". Franny Armstrong, who runs the 10:10 campaign, which is backed by the Guardian, says the topic came up in the planning stages of the project, but was abandoned. "We did have the discussion. But we decided it couldn't work, because of the timescale. 10:10 is a short-term campaign about reductions you can make in 2010."

Besides, a decade after Bill McKibben published Maybe One, we're apparently still not ready to contemplate its message. "10:10 is a populist campaign. It's about doing the easy things first," Armstrong says. "I completely agree that [family size] is the elephant in the room. But we need one of the big thinkers, a George Monbiot or a Naomi Klein, to go first, before anyone else is going to say it. To use that as a message in a populist ­campaign, right now? It would absolutely destroy the whole campaign."

The fundamental problem with the topic of influencing population levels is that almost everybody – no matter what their politics or other beliefs – has a very good reason to avoid discussing it. If you don't believe in climate change, it's yet more irrelevant, busybodyish meddling. If you're broadly leftwing or progressive, as are most people strongly committed to reducing their own environmental impact, it's awkward, because raising the issue seems to shift responsibility from the developed countries, which bear most historical responsibility for climate damage, to the develop­ing world, where population growth is most rapid. And for anti-immigration voices on the right, the whole idea seems backwards: they worry that Europe's population – by which they usually mean its white population – isn't growing fast enough, so promot­ing smaller families is perverse. Above all, perhaps, there's the simple fact that family size seems such an intensely personal matter, beyond the legitimate scope of politics or public campaigns. Just mentioning it feels somehow inappropriate.

There's another awkward truth: historical predictions of catastrophic population explosions have tended to be badly wrong, from Malthus in the 1700s, to Paul Ehrlich in the 1960s, to the UN Population Fund, which predicted in 1987 that a world population of 5bn would mean the world "could degenerate into disaster". (The number is now well over 6.7bn.) Nearly everyone, meanwhile, is troubled by the notion of coercion: China's "one-child policy", promoted by Chinese politicians at Copenhagen as a solution to the climate crisis, has resulted in numerous reports of forced sterilisation and abortion, and rumours of infanticide. Supporters of reproductive choice are understandably appalled. Then again, trying to achieve a similar end by voluntary means, by making family planning more widespread, draws fury from the other side of the spectrum: pro-life campaigners, who fear a surge in abortions.

A recent study by the Optimum Population Trust (OPT) estimated that saving a tonne of CO2 costs only $7 if the money is spent on family planning; to achieve the same by means of solar power would cost $51. The finding paralysed environmental organisations, especially in America, where even the hint of increased funding for abortion carries huge political costs. "I don't know how to say 'no comment' emphatically enough," David Hamilton, of the US green group the Sierra Club, told the Washington Post. (He had reason to be reticent: the Sierra Club suffered its own encounter with the tangled politics of population in 2004 when a group of population-control advocates tried to stage a takeover. On that occasion, just to confuse matters further, those attempting the takeover were fiercely opposed to immigration, on the grounds that immigrants to the US develop bigger carbon footprints once they get there.)

Strictly speaking, though, none of this ought to be relevant to the parenting decisions of the average climate-conscious Briton. Perhaps the OPT is a brave voice in the wilderness – "Nobody else wants to put their head above the parapet," says Simon Ross, an OPT trustee – or perhaps, as George Monbiot says, they're a "congregation of no ones" – a gaggle of post-reproductive white middle-class men trying to shift attention to the one part of the climate problem for which they're not responsible. Either way, from the point of view of climate change, choosing to have one fewer child – especially if you live in a high-consumption society – remains a Very Good Thing Indeed.

And yet even that more narrowly focused topic seems to provoke a surprising degree of fury. Two years ago, Sarah Irving, then a journalist at Ethical Consumer magazine, was one of several people featured in a Daily Mail article on couples who had taken the small-family idea to its logical conclusion, opting to have no children at all. (The Mail article is inadvertently hilarious, so baffled are its authors by the concept of voluntary childlessness; one woman's decision to have an abortion on environmental grounds is described as "the reversal of nature" and "the denial of motherhood".) "There were people who went to the lengths of finding my personal email address to say things like, 'Why don't you just kill yourself?' " Irving says, even though she was specifically quoted in the article as saying she'd never dream of telling other people whether or not to have children. "Generally speaking, if you're talking about having no children at all, you're still regarded as barmy or selfish. Or you get the patronising, 'Oh, you know, you'll change your mind.' "

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Friday, February 12, 2010

Carbon targets pledged at Copenhagen 'fail to keep temperature rise to 2C'

The pledges made by governments resulting from the Copenhagen climate conference are nowhere near enough to hold global temperatures to the summit's agreed goal of no more than a 2C rise, researchers have calculated. The results, which are the most rigorous analyses yet made of pledges submitted to the UN last month, will increase pressure on rich countries to make far deeper cuts in negotiations over the next year.

Researchers from the Sustainability Institute, the MIT Sloan School of Management, and Ventana Systems in the US conclude that emissions reduction pledges would allow global mean temperature to increase approximately 3.9C, a level that could see global warming run out of control. "Under the current proposals, global emissions of greenhouse gases would increase 0.8C a year between now and 2020, , warned the joint report. It concluded that to reach the Copenhagen accord's goal of no more than a 2C rise, global emissions must peak within the next decade and fall to at least 50% below 1990 levels by 2050, which would require emissions cuts of 3% annually after 2020.

"A new degree of collective ambition and cooperation will be required before the world sees a climate agreement consistent with limited warming to even 2C let alone the 1.5C goal named by a growing number of governments and civil society groups," said Elizabeth Sawin of Sustainability Institute in Hartland, Vermont, referring to a push at Copenhagen by the Alliance of Small Island States (Aosis) and 48 developing nations for a deal that limits temperature rises to 1.5C.

"The situation is serious. An increase of temperature of more than 1C above pre-industrial levels would result in the disappearance of our glaciers in the Andes, and the flooding of various islands and coastal zones," said Bolivian foreign minister minister, David Choquehuanca, responding to the US study. Scientists are agreed that an overall rise of 2C in world temperatures would be serious for food production, species loss and freshwater supplies. But anything over 3C would lead to the collapse of the Amazon rainforest, crippling water shortages across South America and Australia and the near-extinction of tropical coral reefs, they have said.

Earlier this week, teams of European researchers from Ecofys, Climate Analytics and the Potsdam Institute in Germany concluded that the pledges made so far if acted upon would lead to a global temperature rising "over" 3C.

The low end of the reduction proposals made by governments at Copenhagen would deliver a reduction of only 2 billion tonnes by 2020, and the best would be nine billion tonnes. However, at least 13-17 billion tonnes of reductions are needed to have more than an even chance of limiting warming to 2C.They said that only two out of 10 developed countries' reduction targets submitted to the Copenhagen accord qualify as "sufficient" to keep global temperature rise below 2C.

In the lead, said the European researchers, were the Maldives and Costa Rica, which have proposed to become "climate-neutral" by around 2020. Also at the ambitious end of the scale are Norway, Japan and Brazil, which are proposing to reduce their emissions significantly.

A third analysis of the pledges of only developed countries, undertaken by the US-based World Resources Institute, concluded that they fall "far short of the range of 25-40% emission reductions [by 2020] that the Intergovernmental Panel on Climate Change says is needed to stabilise concentrations of CO2 equivalent at 450 parts per million ppm" Climate campaigners such as Bill McKibben have been pushing for a limit of 350 ppm.

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Thursday, February 11, 2010

Climate sceptics denounced by Brown as he launches climate change group

Prime minister Gordon Brown today accused climate change sceptics of going "against the grain" of scientific evidence, as he launched a new group to raise billions of pounds for the fight against global warming.

Mr Brown will co-chair the United Nations High Level Advisory Group on Climate Change Financing with Ethiopian prime minister Meles Zenawi.

The group aims to raise $30bn (£19bn) over the next three years - rising to $100bn annually by 2020 – to help poor countries limit their contribution to global warming and adapt to its effects.

Cash raised from state and private sources will fund measures to halt deforestation, encourage low-carbon development and adapt to rising sea levels, extreme weather events and higher temperatures.

Despite the failure to reach a legally-binding compact at the Copenhagen talks in December, Mr Brown today said that he believed sufficient offers were on the table to meet some of the conference's key goals.

"66 countries have set out their plans or targets for climate change, covering 80% of global emissions," he said. "Already we can say that if promises are met, the accord will lead to a peaking of global emissions by or before 2020 and make it possible for us to hold the trajectory of global temperature increases to 2C."

Britain continues to support a legally-binding agreement at the UN conference in Cancun, Mexico, later this year, he said.

The weeks following Copenhagen have seen the science behind climate change come increasingly under attack, following the hacking of researchers' emails and the revelation that an inaccurate assertion about melting glaciers was included in the influential 2007 report by the UN's Intergovernmental Panel on Climate Change.

But Mr Brown brushed aside the sceptics' challenge during a UN webcast to launch the group today.

"Those people who have become global warming deniers and those people who have become climate change deniers are against the grain of all the evidence that has been assembled that global warming and climate change are indeed challenges that the world must meet and that can only be met together," he said. He has previously denounced what he described as "anti-science, flat-earth climate sceptics".

UN Secretary General Ban Ki-moon cautioned against thinking that the cold winter in the northern hemisphere – which is currently causing heavy snowfall in the New York area – disproves the global warming hypothesis.

"It may be true that you have seen some cold weather, as we have seen recently in New York, but the overall tradition of scientific evidence suggests that global warming is happening much faster than one may realise," said Mr Ban.

"That is what I have been told by the scientists and I believe that is true."

Mr Brown said that the group would take on "the task that I believe is the most important we face – combating climate change by ensuring that the poorest countries have the finance necessary to do so".

He added: "If we can resolve this problem then I believe many of the other challenges of climate change can also be solved. The task before us, while daunting, is a very important one to the future of the environment of the world."

Mr Brown said that funds for mitigation and adaptation to climate change must come on top of official development aid, and acknowledged that private sources must be found for some of the money – for instance by auctioning national emissions allowances.

"This can't all be done from taxpayer revenues so we must examine new sources of finance, both public and private," he said.

The PM pledged that Britain would contribute, saying: "Let me stress that the UK is committed to paying its share of the up to $30bn required by developing countries from 2010. We will stand by and make our commitment real to that part of the agreement at Copenhagen."

Asad Rehman, senior international climate campaigner at Friends of the Earth, said: "$10bn a year might sound like a wave of new money for poor countries to tackle climate change, but in reality it's a drop in the ocean compared to what is required. What's worse is that most of this money from rich countries will be plundered from existing aid budgets." Last month the UK government admitted that its £1.5bn contribution to the 2010-2012 funding would be taken from its existing overseas aid budget.

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Wednesday, February 10, 2010

New UN emissions pledges still stack up to 3.5°C

THE Copenhagen climate dance continues. This week, 55 nations representing 78 per cent of global greenhouse gas emissions from energy use, submitted pledges to the UN to cut emissions by 2020.

The commitments were made to meet a deadline set at the climate talks held in Copenhagen in December. But they mostly reiterate national pledges made before the summit, and are steeped in conditions. The US, for instance, reaffirmed its commitment to cut emissions to 17 per cent below 2005 levels, contingent on legislation being passed at home. China repeated that it would "endeavour to lower its carbon dioxide emissions per unit of GDP by 40 to 45 per cent" between 2005 and 2020.

"The vast majority of nations has failed to seize this opportunity to make their pledges more ambitious," says Niklas Höhne, a policy analyst at Ecofys in Cologne, Germany. "Our analysis suggests that the world is still on track for a 3.5 °C rise."

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Tuesday, February 9, 2010

Our world may be a giant hologram

DRIVING through the countryside south of Hanover, it would be easy to miss the GEO600 experiment. From the outside, it doesn't look much: in the corner of a field stands an assortment of boxy temporary buildings, from which two long trenches emerge, at a right angle to each other, covered with corrugated iron. Underneath the metal sheets, however, lies a detector that stretches for 600 metres.

For the past seven years, this German set-up has been looking for gravitational waves - ripples in space-time thrown off by super-dense astronomical objects such as neutron stars and black holes. GEO600 has not detected any gravitational waves so far, but it might inadvertently have made the most important discovery in physics for half a century.

For many months, the GEO600 team-members had been scratching their heads over inexplicable noise that is plaguing their giant detector. Then, out of the blue, a researcher approached them with an explanation. In fact, he had even predicted the noise before he knew they were detecting it. According to Craig Hogan, a physicist at the Fermilab particle physics lab in Batavia, Illinois, GEO600 has stumbled upon the fundamental limit of space-time - the point where space-time stops behaving like the smooth continuum Einstein described and instead dissolves into "grains", just as a newspaper photograph dissolves into dots as you zoom in. "It looks like GEO600 is being buffeted by the microscopic quantum convulsions of space-time," says Hogan.

If this doesn't blow your socks off, then Hogan, who has just been appointed director of Fermilab's Center for Particle Astrophysics, has an even bigger shock in store: "If the GEO600 result is what I suspect it is, then we are all living in a giant cosmic hologram."

The idea that we live in a hologram probably sounds absurd, but it is a natural extension of our best understanding of black holes, and something with a pretty firm theoretical footing. It has also been surprisingly helpful for physicists wrestling with theories of how the universe works at its most fundamental level.

The holograms you find on credit cards and banknotes are etched on two-dimensional plastic films. When light bounces off them, it recreates the appearance of a 3D image. In the 1990s physicists Leonard Susskind and Nobel prizewinner Gerard 't Hooft suggested that the same principle might apply to the universe as a whole. Our everyday experience might itself be a holographic projection of physical processes that take place on a distant, 2D surface.

The "holographic principle" challenges our sensibilities. It seems hard to believe that you woke up, brushed your teeth and are reading this article because of something happening on the boundary of the universe. No one knows what it would mean for us if we really do live in a hologram, yet theorists have good reasons to believe that many aspects of the holographic principle are true.

Susskind and 't Hooft's remarkable idea was motivated by ground-breaking work on black holes by Jacob Bekenstein of the Hebrew University of Jerusalem in Israel and Stephen Hawking at the University of Cambridge. In the mid-1970s, Hawking showed that black holes are in fact not entirely "black" but instead slowly emit radiation, which causes them to evaporate and eventually disappear. This poses a puzzle, because Hawking radiation does not convey any information about the interior of a black hole. When the black hole has gone, all the information about the star that collapsed to form the black hole has vanished, which contradicts the widely affirmed principle that information cannot be destroyed. This is known as the black hole information paradox.

Bekenstein's work provided an important clue in resolving the paradox. He discovered that a black hole's entropy - which is synonymous with its information content - is proportional to the surface area of its event horizon. This is the theoretical surface that cloaks the black hole and marks the point of no return for infalling matter or light. Theorists have since shown that microscopic quantum ripples at the event horizon can encode the information inside the black hole, so there is no mysterious information loss as the black hole evaporates.

Crucially, this provides a deep physical insight: the 3D information about a precursor star can be completely encoded in the 2D horizon of the subsequent black hole - not unlike the 3D image of an object being encoded in a 2D hologram. Susskind and 't Hooft extended the insight to the universe as a whole on the basis that the cosmos has a horizon too - the boundary from beyond which light has not had time to reach us in the 13.7-billion-year lifespan of the universe. What's more, work by several string theorists, most notably Juan Maldacena at the Institute for Advanced Study in Princeton, has confirmed that the idea is on the right track. He showed that the physics inside a hypothetical universe with five dimensions and shaped like a Pringle is the same as the physics taking place on the four-dimensional boundary.

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Sunday, February 7, 2010

Sun-powered water splitter makes hydrogen tirelessly

Sunlight + water = hydrogen gas, in a new technique that can convert 60 per cent of sunlight energy absorbed by an electrode into the inflammable fuel.

To generate the gas Thomas Nann and colleagues at the University of East Anglia in Norwich, UK, dip a gold electrode with a special coating into water and expose it to light. clusters of indium phosphide 5 nanometres wide on its surface absorb incoming photons and pass electrons bearing their energy on to clusters of a sulphurous iron compound.

This material combines those electrons with protons from the water to form gaseous hydrogen. A second electrode – plain platinum this time – is needed to complete the circuit electrochemically.

Organic molecules have been used before to perform the same feat. But they are quickly bleached by the sunlight they are collecting, rendering them inefficient after a few weeks.

The inorganic materials used in the University of East Anglia's system are more resilient. Their first generation proof of concept is "a major breakthrough" in the field, they say, thanks to its efficiency of over 60 per cent and ability to survive sunlight for two weeks without any degradation of performance.

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Saturday, February 6, 2010

Climategate inquiry stumbles on the start line

One day in, and already one of the five reviews into "climategate" has been hit by its own controversy.

Former civil servant Muir Russell will head an independent inquiry into the professional behaviour of climate scientists at University of East Anglia (UEA) in Norwich, UK, relating to the emails which were leaked into the public domain last November.

Russell, whose career was devoted to the government of Scotland, announced his panel of six independent experts yesterday. Hours later, one of them – Philip Campbell, editor of Nature – was forced to step down over claims that he is not impartial: last year, Campbell told a Chinese radio station that there was nothing to suggest that the UEA scientists had misbehaved.

"I made the remarks in good faith, on the basis of media reports of the leaks. As I have made clear subsequently, I support the need for a full review of the facts behind the leaked emails," Campbell said yesterday.
Investigation remit

Russell's review will investigate whether the UEA emails – which were leaked on the web last November – demonstrated that the UEA scientists were guilty of "manipulation or suppression of data".

It will also investigate whether the scientists thwarted freedom of information legislation and whether the UEA Climatic Research Unit's policies for "acquiring, assembling, subjecting to peer review and disseminating data and research findings" met best scientific practice. The research unit is at the centre of the email scandal.

Russell said the panel would not investigate the validity of the unit's scientific findings. Its preliminary findings should be published "by the spring".

At the announcement of the panel yesterday, Russell insisted that, though its work would be funded by UEA, it was independent. Journalists asked Campbell whether he had a conflict of interests, given that his journal has published papers by UEA scientists such as director Phil Jones and used UEA scientists to review submitted papers; Campbell denied it.

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Friday, February 5, 2010

Protection of the ozone layer



Introduction

The ozone layer is a layer of gas in the upper atmosphere which protects humans and other living things from the harmful ultraviolet (UV-B) rays of the sun. In the 1970s scientists discovered that certain man-made chemicals could destroy ozone and deplete the ozone layer. Further research found that the growing production and use of chemicals like chlorofluorocarbons (CFCs) in aerosol sprays, refrigeration, insulation and air conditioning was contributing to the accumulation of ozone-depleting substances (ODS) in the atmosphere. They also observed that an ‘ozone hole’ was developing above the Antarctic. Find here more

information about the ozone hole.

A thinning ozone layer leads to a number of serious health risks for humans. It causes greater incidences of skin cancer and cataract of the eye, with children being particularly vulnerable. There are also serious impacts for biodiversity. Increased UV-B rays reduce levels of plankton in the oceans and subsequently diminish fish stocks. It can also have adverse effects on plant growth, thus reducing agricultural productivity. Another negative effect is the reduced lifespan of certain materials.

Severe depletion of the Antarctic ozone layer was first observed in the early 1980s. The international response embodied in the Montreal Protocol. Today 191 countries worldwide have signed the Montreal Protocol which is widely regarded as the most successful Multinational Environmental Agreement ever reached to date.

Furthermore the phasing out of ozone depleting substances (ODS) has helped to fight climate change since many ODS are also powerful greenhouse gases.

The ozone layer protection policy of the EU and its Member States is even more ambitious than the Montreal Protocol.

While the Montreal Protocol has made great strides in the global effort to protect the ozone layer, the task is far from being complete. Despite all efforts substantial recovery of the ozone layer is not expected before the middle of the 21st century.

Hence there is the need for new impetus on negotiations to fight the challenges still ahead.

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Thursday, February 4, 2010

A post-2012 global climate regime: the EU's contribution

International negotiations are under way to draw up a United Nations climate change agreement for the period after 2012, when the first commitment period of the Kyoto Protocol expires.

The European Union has long been in the vanguard of international action to combat climate change. For the EU, the international negotiations must result in a legally binding global treaty that is comprehensive, ambitious, fair and science-based.

The treaty should aim to keep global warming below 2°C above the pre-industrial temperature, or around 1.2°C above today's level (see brochure). The treaty should cover all elements of the 2007 Bali Action Plan, which set the agenda and scope of the international negotiations.

Scientific evidence shows that to keep within the 2°C ceiling, global emissions of greenhouse gases will have to peak by 2020 at the latest, be cut by at least 50% of their 1990 levels by 2050, and continue to decline thereafter.

These objectives can be achieved only through a worldwide effort involving developed and developing countries alike.

Industrialised nations must take the lead by making deep emission cuts of 25-40% below 1990 levels by 2020 and of 80-95% by 2050.

Action by developing nations (except the least developed countries) will also be needed to limit the rapid growth in their emissions. In particular the more economically advanced developing countries should pledge ambitious, quantified mitigation actions.

Overall, developing country pledges need to amount to a substantial deviation - in the order of 15-30% - below the currently predicted growth rate in their collective emissions by 2020. The EU is ready to provide its fair share of financial assistance to help developing countries mitigate their emissions and adapt to climate change.

The EU considers the Copenhagen Accord, negotiated at the UN climate conference in Copenhagen in December 2009, as a first step towards a legally binding global climate agreement. The EU has formally notified its willingness to be associated with the Accord and submitted its emission reduction targets. The EU's goal is to reach a legally binding global agreement at the earliest opportunity.

The EU's position on post-2012 global action is set out in two sets of 'conclusions' representing the views of the Council of EU Environment Ministers and of the European Council (which brings together the EU Heads of State and Government).

The EU position has been shaped by a series of policy papers ("Communications") from the European Commission. These papers have also served to stimulate international debate. The Communications are presented

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Wednesday, February 3, 2010

Debate heats up over IPCC melting glaciers claim

Glaciologists are this week arguing over how a highly contentious claim about the speed at which glaciers are melting came to be included in the latest report of the Intergovernmental Panel on Climate Change.

In 1999 New Scientist reported a comment by the leading Indian glaciologist Syed Hasnain, who said in an email interview with this author that all the glaciers in the central and eastern Himalayas could disappear by 2035.

Hasnain, of Jawaharlal Nehru University in Delhi, who was then chairman of the International Commission on Snow and Ice's working group on Himalayan glaciology, has never repeated the prediction in a peer-reviewed journal. He now says the comment was "speculative".



Despite the 10-year-old New Scientist report being the only source, the claim found its way into the IPCC fourth assessment report published in 2007. Moreover the claim was extrapolated to include all glaciers in the Himalayas.

High probability

Chapter 10 of the report says: "Glaciers in the Himalaya are receding faster than in any other part of the world."

The inclusion of this statement has angered many glaciologists, who regard it as unjustified. Vijay Raina, a leading Indian glaciologist, wrote in a discussion paper published by the Indian government in November that there is no sign of "abnormal" retreat in Himalayan glaciers. India's environment minister, Jairam Ramesh, accused the IPCC of being "alarmist".

The IPCC's chairman, Rajendra Pachauri, has hit back, denouncing the Indian government report as "voodoo science" lacking peer review. He adds that "we have a very clear idea of what is happening" in the Himalayas.

'Disturbing' prediction

The IPCC report sources the prediction to a document published by the environment group WWF in 2005; this document quotes the New Scientist article as its source. The WWF report describes the prediction as "disturbing", without specifically endorsing it.

Nonetheless, the IPCC report goes further, concluding without citing further evidence that the prediction is "very likely" – a term that it says means a likelihood of greater than 90 per cent.

Graham Cogley, a geographer from Trent University in Peterborough, Ontario, Canada, says the 2035 date is extremely unlikely. "At current melting rates it might take up to 10 times longer," he says.

Grey literature

However, the lead author of the IPCC chapter, Indian glaciologist Murari Lal, told New Scientist he "outright rejected" the notion that the IPCC was off the mark on Himalayan glaciers. "The IPCC authors did exactly what was expected from them," he says.

"We relied rather heavily on grey [not peer-reviewed] literature, including the WWF report," Lal says. "The error, if any, lies with Dr Hasnain's assertion and not with the IPCC authors."

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Conclusion

Current warming trends are unequivocal. It is very likely that greenhouse gases released by human activities are responsible for most of the warming observed in the past fifty years. The warming is projected to continue and to increase over the course of the 21st century and beyond.

Climate change already has a measurable impact on many natural and human systems. Effects are projected to increase in the future and to be more severe with greater increases in temperature. Adaptation measures are already being implemented, and will be essential in order to address the projected consequences. There is, however, a limit to adaptation; mitigation measures will also be needed in order to reduce the severity of impacts.

Mitigation measures that aim to reduce greenhouse gas emissions can help avoid, reduce or delay many impacts of climate change. Policy instruments could create incentives for producers and consumers to significantly invest in products, technologies and processes which emit less greenhouse gases. Without new mitigation policies, global greenhouse gas emissions will continue to grow over the coming decades and beyond. Rapid world-wide investments and deployment of mitigation technologies, as well as research into new energy sources will be necessary to achieve a stabilization of the concentration of greenhouse gases in the atmosphere.

Additional research addressing gaps in knowledge would further reduce uncertainties and thus facilitate decision-making related to climate change.

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How can governments create incentives for mitigation?

  • 9.1 What are the implications of different policy instruments?
  • 9.2 How is climate change mitigation linked to sustainable development?

9.1 What are the implications of different policy instruments?

A wide variety of policy tools can be applied by governments to create incentives for mitigation action taking into account national circumstances and interactions between policies. Experience from various countries and sectors shows there are advantages and drawbacks for any given policy instrument. It is important to consider environmental effectiveness of policies and instruments, their cost effectiveness, institutional feasibility and how costs and benefits are distributed.

Examples of policies and instruments:

  • Integrating climate policies into broader development policies makes implementation easier.
  • Regulations and standards generally provide some certainty about emission levels, but they may not encourage innovation and the development of new technologies.
  • Taxes and charges can set a “carbon price” (a cost for each unit of greenhouse gas emissions) and be an effective mitigation incentive, but cannot guarantee a particular level of emissions.
  • Tradable emission permits establish a “carbon price”. The volume of allowed emissions determines their environmental effectiveness, while the way permits are allocated determines who bears the costs. Fluctuation in the “carbon price” makes it difficult to estimate the total cost of complying with emission permits.
  • Subsidies and tax credits can provide financial incentives for the development and diffusion of new technologies. Though sometimes costly, they are often critical to overcome barriers.
  • Voluntary agreements between industry and governments are politically attractive, raise awareness, and have played a role in the evolution of many national policies. Only a few of them have led to measurable emission reductions.
  • Awareness campaigns may positively affect environmental quality by promoting informed choices and possibly contributing to behavioural change. However, their impact on emissions has not been measured yet.
  • Research, Development and Demonstration (RD&D) can stimulate technological advances, reduce costs, and enable progress toward stabilization.

Economic instruments, government funding or regulation that lead to a “carbon price” (a cost for each unit of greenhouse gas emissions) could create incentives for producers and consumers to significantly invest in products, technologies and processes reduce greenhouse gas emissions.

Government support through financial contributions, tax credits, standard setting and market creation is important for effective technology development, innovation and deployment. Effective transfer of technology to developing countries requires appropriate financial, institutional, policy, legal and regulatory frameworks.

9.2 How is climate change mitigation linked to sustainable development?

Switching to more sustainable development paths can make a major contribution to climate change mitigation, but implementation may require overcoming multiple barriers. Climate change and other sustainable development policies often benefit each other, though not always. There is a growing understanding of the possibilities to choose and implement mitigation options in several sectors to create synergies and avoid conflicts with other aspects of sustainable development.

For instance, climate change policies related to energy efficiency and renewable energy are often economically beneficial, improve energy security, and reduce local air pollution. Reducing both loss of natural habitat and deforestation can have significant benefits for biodiversity, soil and water conservation, and can be implemented in a socially and economically sustainable manner.

No matter how stringent the mitigation measures, some impacts of climate change are unavoidable and adaptation will be necessary. Sustainable development can increase the capacity for both adaptation and mitigation, and reduce vulnerability to the impacts of climate change.

Gaps in knowledge remain regarding some aspects of mitigation of climate change, especially in developing countries. Additional research addressing those gaps would further reduce uncertainties and thus facilitate decision-making related to mitigation of climate change.

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What actions can be taken to reduce greenhouse gas emissions?

8.1 Mitigation measures to reduce greenhouse gas emissions have a certain cost. However, they also constitute an economic benefit by reducing the impacts of climate change, and the costs associated with them. In addition, they can bring economic benefits by reducing local air pollution and energy resource depletion.

If the benefits of avoided climate change are taken into account and a “carbon price” is established for each unit of greenhouse gas emissions, this could create incentives for producers and consumers to significantly invest in products, technologies and processes which emit less greenhouse gases. The resulting mitigation potential is substantial and could offset the projected growth of global emissions over the coming decades or reduce emissions below current levels.

Mitigation measures could contribute to stabilizing the concentration of greenhouse gases in the atmosphere by 2100 or later. To achieve low stabilization levels, stringent mitigation efforts are needed in the coming decades. This could reduce global GDP by up to a few percent.

8.2 Changes in lifestyle and behaviours that favor resource conservation can contribute to climate change mitigation.

8.3 Mitigation measures can also have other benefits for society, such as health cost savings resulting from reduced air pollution. However, mitigation in one country or group of countries could lead to higher emissions elsewhere or effects on the global economy.

8.4 No one sector or technology can address the entire mitigation challenge. All sectors including buildings, industry, energy production, agriculture, transport, forestry, and waste management could contribute to the overall mitigation efforts, for instance through greater energy efficiency. Many technologies and processes which emit less greenhouse gases are already commercially available or will be in the coming decades.

8.5 In order to stabilize the concentration of greenhouse gases in the atmosphere, emissions would have to stop increasing and then decline. The lower the stabilization level aimed for, the more quickly this decline would need to occur. World-wide investments in mitigation technologies, as well as research into new energy sources, will be necessary to achieve stabilization. Delaying emission reduction measures limits the opportunities to achieve low stabilization levels and increases the risk of severe climate change impacts.

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What are the current trends in greenhouse gas emissions?

Since pre-industrial times, increasing emissions of greenhouse gases due to human activities have led to a marked increase in the concentration of greenhouse gases in the atmosphere. Between 1970 and 2004, global emissions have increased by 70%. Over this period, emissions from the energy and transport sectors have more than doubled.

Global greenhouse gas emissions include carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), and fluorinated greenhouse gases (HFCs, PFCs and SF6). The gases are each weighted by their global warming potential and the total is expressed in Gigatonnes of carbon dioxide equivalents (GtCO2-eq). In 2004, total greenhouse gas emissions due to human activities reached 49 Gigatonnes of carbon dioxide equivalents (GtCO2-eq) and CO2 alone represented 77% of the total.

Although since the 1970s less and less energy is needed to generate a given amount of GDP, this decrease has been offset by the global economic and population growth. Emission reduction policies have been put in place in some countries that have been effective in reducing emissions in those countries to a certain degree, but not sufficiently to counteract the global growth in emissions.

With current mitigation policies and sustainable development practices alone, global greenhouse gas emissions will continue to grow. Indeed, in the absence of additional mitigation measures, emission scenarios project an increase of 25 to 90% in greenhouse gas emissions in 2030 compared to 2000. (See The Emission Scenarios of the IPCC)

Fossil fuels are expected to maintain their dominant position in the global energy mix beyond 2030. Hence between 2000 and 2030, CO2 emissions from energy use are projected to grow 45 to 110% over that period, particularly in developing regions (non-Annex I regions). CO2 emissions per capita are expected to remain substantially higher in developped countries compared to the rest of the world (Annex I regions). However, developed countries are expected to use less energy per unit of GDP than developing countries.

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How do people adapt to climate change?

  • 6.1 What are the current adaptation strategies?
  • 6.2 What makes populations vulnerable to climate change?
  • 6.3 What are the relative roles of mitigation and adaptation?

6.1 What are the current adaptation strategies?

Some adaptation of human activities to both observed and anticipated climate change is already taking place. For instance, climate change is taken into account in coastal defense projects in the Maldives and the Netherlands. Other examples include prevention of glacial lake outburst flooding in Nepal, water management strategies in Australia, and government responses to heat waves in some European countries.

Past emissions are expected to cause some unavoidable warming (about a further 0.6°C by the end of the century) even if the amount of greenhouse gas concentrations in the atmosphere remained at the same level as they were in the year 2000. There are thus some impacts for which adaptation is the only option.

Although many early impacts of climate change can be effectively addressed through adaptation, the options for successful adaptation diminish and the associated costs increase with increasing climate change.

A wide array of adaptation options exist, including technological solutions such as coastal defenses, behaviour changes such as the modification of consumption habits, as well as policy and managerial solutions. While the limits to adaptation are not yet known, it is not expected that adaptation alone will be sufficient to cope with all projected impacts as they increase in magnitude.

6.2 What makes populations vulnerable to climate change?

The vulnerability of natural environments and human societies to climate change can be exacerbated by factors such as poverty, pollution, conflicts, or epidemics such as AIDS.

Future vulnerability will depend not only on the changes in climate but also on the development path chosen. Indeed different development scenarios foresee large differences in regional population, income and technological development, which strongly affect vulnerability to climate change.

A sustainable approach to development, for instance, can help reduce vulnerability to climate change by increasing the capacity of populations to adapt. However, climate change itself can become an obstacle to development, slowing down progress and potentially preventing the achievement of the Millennium Development Goals (MDG).

6.3 What are the relative roles of mitigation and adaptation?

Many impacts can be avoided, reduced or delayed by mitigation, which mainly aims to reduce greenhouse gase emissions. However even the most severe mitigation measures cannot completely avoid impacts of climate change in the next few decades. Measures to adapt to impacts also have their limits.

There is therefore a need for or mix of strategies that includes mitigation, adaptation, technological development (to enhance both adaptation and mitigation) and research (on climate science, impacts, adaptation and mitigation).

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What is the magnitude of expected impacts?

Thanks to recent data, the magnitude of impacts can now be better estimated for possible increases in global average temperature. Impacts are expected to increase with temperature, as indicated in Figure SPM-2.For instance:

  • Some crops will have better productivity if temperatures increase by 1 to 2°C, but if temperatures rise by 3-4°C, those same crops will be negatively affected.
  • Coral reefs are already affected by small global temperature increase. They would further suffer if temperatures increased by 1 to 2°C, and many would die if it increased by 2.5°C.

If warm temperatures persist after the 21st century, it could result in very large impacts. For instance, the large sea-level rise (up to 12 m) that would result from the melting of the Greenland and Antarctic ice sheets would have major impacts on coastal areas, with effects both on biological systems and human populations.

It is very unlikely that the North Atlantic Ocean circulation that gives rise to the Gulf Stream will undergo a large abrupt transition during the 21st century. A slowing of this circulation is very likely over this century, but temperatures over the Atlantic and Europe are projected to increase nevertheless, due to global warming.

Global mean losses could be 1-5% of the world Gross Domestic Product (GDP) for 4°C of warming, with larger percentage losses in developing countries (Note: 1% represented US$ 650 billion in 2006).

Many estimates of net costs of damages from climate change across the globe are now available. The average estimate for 2005 was US$12 per tonne of carbon dioxide with a large variability between estimates. Such global cost estimates tend to mask significant differences across sectors, regions, countries, and populations. In some locations and amongst some groups net costs will be significantly larger.

Overall, the published evidence indicates that the net cost of climate change is likely to be significant and to increase as global temperatures increase.

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What impacts of climate change have already been observed?

In all regions of the world observations show that many natural systems are being affected by regional climate change, particularly by temperature increases.

Snow and ice are melting and frozen ground is thawing. The number of glacial lakes is increasing and so is ground instability in permafrost regions. The flow of rivers that are fed by melting snow and glaciers has increased, and the temperature of lakes and rivers has risen. Spring events such as migrations are starting earlier and the geographical spread of species is extending towards the poles. In addition, the CO2 emitted by human activities has caused an increase of ocean acidity, with poorly understood but potentially important negative impacts.

Evidence accumulated over the past five years indicates that changes in many physical and biological systems are linked to the warming caused by human activities.

* Most of the warming observed since 1950 is very likely due to the increase of greenhouse gases generated by human activities.
* In most cases, when long term measurements revealed significant environmental change, the change went in the direction that would be expected as a result of a warming climate.
* Regions with significant changes are also the ones experiencing significant warming.
* Model projections have linked the changes in some physical and biological systems to the warming induced by human activities.

Despite limitations and gaps in knowledge, there is sufficient evidence to conclude with high confidence that over the last three decades the warming induced by human activities has had a measurable impact on many physical and biological systems.

Some impacts of regional climate change are only emerging at this stage. They remain difficult to discern because they also depend on factors other than climate or because some adaptation has taken place. Temperature increases could for instance already have affected agricultural and forest management, the number of heat related deaths, the spread of vectors of disease such as insects carrying malaria.

Recent changes are beginning to have effects, for instance mountain settlements are at risk of floods due to melting glaciers, the growing season in the Sahelian region of Africa is shortening, and damage from coastal flooding is increasing

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What changes are projected on the longer term?

Temperatures are projected to increase by 1.8°C to 4.0°C.
From 1980 to the end of the 21st century, temperatures are projected to increase by 1.8°C to 4.0°C.

Warming and sea level rise caused by human activities will continue for centuries, even if greenhouse gas concentrations were to be stabilized, because of the long timescales associated with climate processes and feedbacks.

Warming is expected to affect the carbon cycle, resulting in even higher carbon dioxide concentration in the atmosphere, but the magnitude of this is uncertain.

If greenhouse gas concentrations in the atmosphere were to stabilize in 2100 at levels projected in the B1 and A1B emission scenarios, a further increase in global average temperature of about 0.5°C would still be expected around 2200. Under this A1B scenario, the thermal expansion of the oceans alone would lead to an increase of 30 to 80 cm of global sea level by 2300, and this rise would continue over many centuries after that.

The melting of the Greenland ice sheet is projected to continue and to contribute to sea level rise after 2100. If it were to keep melting for millennia until Greenland ice disappeared completely, global sea level would rise by about 7m.

The vulnerability of the ice sheets to warming could be increased by dynamical processes related to ice flow (not included in current models but suggested by recent observations) thereby increasing future sea level rise. Current global model studies project that the Antarctic ice sheet will remain too cold for widespread surface melting and is expected to gain in mass due to increased snowfall.

Both past and future human emissions of carbon dioxide will continue to contribute to warming and sea level rise for more than a millennium, due to the long time it takes for this gas to disappear from the atmosphere

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What is causing the present-day changes in climate?

It is very likely that a significant part of temperature variability in the Northern hemisphere during the past seven centuries prior to 1950 is due to volcanic eruptions and changes in the intensity of solar radiation. However, most of the observed increase in global temperature since then is very likely due to the observed increase in atmospheric greenhouse gas concentrations due to human activities. Human activities now clearly affect other aspects of climate, including ocean warming, continental-average temperatures, temperature extremes and wind patterns.

It is likely that these increases in greenhouse gas concentrations alone would have caused more warming than observed, had volcanic and human-induced aerosols not offset some of the warming that would otherwise have taken place.

Current climate models that simulate the observed temperature evolution on each of six continents provide stronger evidence of human influence on climate than was available in the 2001 Third Assessment Report (TAR). Difficulties remain in simulating temperature changes at smaller scales, where natural climate variability is larger and makes it harder to estimate the current and future impact of greenhouse gas increases due to human activities.

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What makes the climate change?

The Earth’s climate is influenced by many factors, such as the amount of greenhouse gases and aerosols in the atmosphere, the amount of energy coming from the sun or the properties the Earth’s surface. Changes in those factors, through human-related or natural processes, have a warming or a cooling effect on the planet because they alter how much of this solar energy is retained or reflected back to space.

The concentrations in the atmosphere of greenhouse gases such as carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) have all increased markedly since 1750, and now exceed by far their pre-industrial levels.

Carbon dioxide is the most important anthropogenic greenhouse gas. Its concentration in the atmosphere (379 ppm in 2005) is now far higher than the natural range over the last 650 000 years (180 to 300 ppm) and is growing faster than ever since the beginning of its continuous direct measurement in 1960, mainly due to fossil fuel use and to a lesser extent to land use change. For instance, emissions of carbon dioxide from fossil fuel use increased from 6.4 Gt per year in the 90s to 7.2 Gt of carbon per year over the period 2000-2005. Concentrations of methane and nitrous oxide in the atmosphere have also greatly increased since pre-industrial times, and those increases are mostly due to human activities such as agriculture and fossil fuel use.

The effect on climate of each of the different drivers is expressed in terms of “radiative forcing”, with positive forcing causing a warming of the surface and negative forcing a cooling of it. The overall effect of human activities since 1750 is very likely (> 90% certainty) to be one of warming, with an estimated increase of energy, or radiative forcing, of 1.6 Watt per square meter over the whole planet. The relative contribution of various factors can be seen in figure 2. The main warming drivers are the various greenhouse gases and it is likely that the warming that they cause has been increasing during the industrial era at a higher rate than at any time over the last 10 000 years. The main cooling drivers are aerosols and the changes in cloud cover that they cause.

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Tuesday, February 2, 2010

Errors and lies thrive in cold weather

HERE'S the question to put to all those who confidently declare that the recent severe winter conditions prove that global warming is nonsense: "Next time there's a heatwave in summer or an unusually mild spell in winter, will you publicly accept that the 'warmists' were right all along? If not, why not? If a cold snap means the climate is getting colder, surely a spell of hot weather proves it is getting warmer?"

The point, of course, is that a bout of extreme weather does not prove anything about climate change. Climate is the average weather over decades.




That said, it is perfectly reasonable to ask why, if the world is warming, have so many places in the northern hemisphere been experiencing record lows? The answer is that for the past few decades cold Arctic air has mostly stayed in the Arctic over winter, trapped by strong winds spinning around the pole. This winter the vortex has weakened and in many places cold air is spilling further south than usual.

The result has been freezing weather for places as far afield as Florida, China and the UK. However, the Arctic, Greenland, much of the Mediterranean and southern Asia have been warmer than usual. So overall the northern hemisphere winter may be no colder than in previous years, it's just that the heat is distributed differently. Indeed, the average surface temperature of the entire planet during January may yet turn out to be one of the warmest on record.

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Sunday, January 31, 2010

Let the sunlight in on climate change

LET'S hear it for the Intergovernmental Panel on Climate Change. A big round of applause, please. Really. It has done amazing, Herculean work.

The IPCC was tasked by the governments of the world to deliver an encyclopedic consensus on the state of knowledge about one of the most far-reaching yet divisive questions of our time. And this grouping of thousands of scientists, taking time out from their regular jobs has, for more than two decades, delivered. Thanks to the IPCC's work, the world's nations have come together to decide that we must prevent our planet warming by more than 2 °C - even if achieving that goal is proving difficult, to say the least.




The serious error, reported here two weeks ago, that led to the inclusion in an IPCC report of mistaken claims about how fast Himalayan glaciers are melting is undoubtedly damaging to the panel's reputation. But it does not in any way undermine the conclusion that human-induced climate change is happening, is dangerous and requires urgent action.

However, the IPCC's heroic days are probably over. The case for anthropogenic climate change has been established; the Nobel prize is won. So it is time for a rethink of where the IPCC is going, and what its future role should be. Two years ago, in the aftermath of the last major assessment report, many scientists argued that the task should have begun then. It is no less urgent now.

We still need the IPCC to serve as a seeker of truth whose deliberations are open to scrutiny. There is plenty of new science to assess. But it makes little sense to have to wait six years between assessments: though reflection, and time for the replication of findings, are essential, why not have an annual report?

The organisation also needs to be more focused on providing the science that will address emerging policy challenges. Its best recent work is in its special reports on topics such as aircraft emissions. A special report on geoengineering would be invaluable, as would a dispassionate assessment of how to measure and verify national greenhouse gas emissions, and carbon sinks such as soils and forests.

Should the IPCC remain as an intergovernmental body - in other words, answerable to national governments from around the world? Yes, it probably should. It was the US, during the Reagan presidency back in the 1980s, that insisted on this. At the time, many scientists were dismayed, fearing political interference in the panel's published reports. But these fears largely failed to materialise, and the fact that national governments all sign off each report has reinforced the IPCC's authority. But public attitudes to science are changing. The IPCC was established before the internet revolution. Like it or not, its closed world of peer review is no longer possible, let alone desirable.

The job of scientists is to test theories to destruction, which inevitably makes science adversarial at times. Dispute is good; consensus stultifies. It is neither surprising nor disturbing that disputes about the science break out, within the IPCC and outside it, and such disagreements need to be out in the open.

Many scientists were unhappy about what they saw as excessive caution in the last assessment - reflected, for instance, in under-reporting of emerging science on how disintegrating polar ice sheets might accelerate sea level rise beyond anything yet revealed in climate models. Such argument should be open to public view. A wider discussion of the uncertainties here would have been more honest and avoided giving a false reassurance.

So let the IPCC embrace such debates, rather than retreat from them in the name of spurious consensus. Climate scientists have felt under siege from critics, as leaked emails last year amply demonstrated. But that is no reason to dismiss all criticism as necessarily unwarranted, uninformed or politically motivated.


Some argue that the views of an untutored blogger, or even a scientist from another discipline, should never carry the same weight as those of someone with a lifetime's expertise in a relevant field. But if occasionally the emperors of the lab have no clothes, someone has to say so. The wider review of science made possible by the blogosphere can improve science and foster public confidence in its methods. Scientists should welcome the outside world in to check them out. Their science is useless if no one trusts it.

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Saturday, January 30, 2010

The clash of two worlds in the Peruvian Amazon

The clash of two worlds in the Peruvian Amazon
The Peruvian government chose the symbolic date of World Environment Day to launch a bloody attack on the peoples of the Amazon. The reason for this repression? The steadfast opposition of Amazonian communities to the invasion of their territory by socially and environmentally destructive industries such as mining, oil drilling, and monoculture plantations of trees and agrofuel crops.


On 9 April local communities throughout the Peruvian Amazon had begun what they called an “indefinite strike” in protest against the failure of the Peruvian Congress to review a series of legislative decrees that endanger the rights of indigenous peoples. These decrees were issued by the executive branch in the framework of the implementation of the Free Trade Agreement signed with the United States.

By unleashing this massacre on World Environment Day, Alan García’s government showed the world how little concern it has for environmental protection and how highly it values the large corporations that hope to exploit – and simultaneously destroy – the country’s natural resources. Even worse, it publicly declared its contempt for the lives of the indigenous people struggling to defend what little has been left to them by the advance of a “development” model that has proved to be socially and environmentally destructive.

As a result of this bloody repression and the public attention it attracted worldwide, the Peruvian Amazon became a symbol of the clash between two different conceptions of the present and future of humanity, played out on the international stage.

On one side of this conflict there is the world of economic interest, which signifies social and environmental destruction, imposition by force, violation of rights. Obviously, this world is not controlled by the Peruvian president, who is merely a temporary and disposable assistant to the corporations – a fact now made evident by the fate of ex-president Fujimori. Nevertheless, the role played by these assistants is very important, since they are the ones who lend the necessary trappings of “legality” to actions that clearly violate the most basic human rights.

On the other side there is the world of those who aspire to a future of solidarity and respect for nature. In this case, they were symbolised by the indigenous people of the Amazon, but they can also be found in similar struggles around the world, confronting other governments who are also at the service of the economic interests of big corporations. To mention just a few examples, we could point to the current struggle in south-east Asian countries to defend the Mekong river – which provides sustenance for millions of people – from destruction by giant hydroelectric dams; the struggle of the peoples of Africa against oil-drilling and logging; the struggle of the tribal peoples of India to protect their forests from mining.

In this confrontation, the hypocrisy of those striving to impose the destructive model seems unbounded. In the case of Peru, President Alan García, who now wants to open up the Amazon to extractive industries, declared just over a year ago that he wanted “to prevent this basic wealth that God has given us from being degraded by the works of man, by the incompetence of those who work the land or exploit it economically, and that is why we created this Ministry of the Environment.”

Governmental hypocrisy is evident all around the world, especially with regard to climate change. During an endless international process that began in 1992, the governments of the world agreed that climate change is the worst threat facing humankind. They also agreed that the two main causes of climate change are greenhouse gas emissions created by the use of fossil fuels and deforestation. Finally, they agreed that something must be done about it. After signing the relevant agreements and flying back to their countries, they have done everything in their power to promote oil-drilling and/or deforestation.

Without needing to create ministries of the environment or participate in international processes to combat climate change, people around the world are taking action to defend the environment and the climate. In almost all cases, their actions are criminalised or repressed – in both the South and the North – by those who should be encouraging and supporting them: their governments.

In the now symbolic case of Peru, the peoples of the Amazon – with the support of thousands of citizens around the world – have won an important battle in this clash between two worlds. No one believes that this is the end of the struggle. But it is a victory that provides hope for others fighting for similar goals, and ultimately for the whole world, because the outcome of this confrontation between two worlds will determine the fate of all of humanity.

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Friday, January 29, 2010

Five key steps towards a food system that can address climate change and the food crisis

Five key steps towards a food system that can address climate change and the food crisis

  • Move towards sustainable, integrated production methods

The artificial separations and simplifications that industrial agriculture has brought upon us have to be undone, and the different elements of sustainable farming systems must be brought together again. Crops and livestock have to be reintegrated on the farm. Agricultural biodiversity has to become the cornerstone of food production again, and local seed saving and exchange systems need to be reactivated. Chemical fertilisers and pesticides must be replaced by natural ways of keeping soil healthy, and pests and diseases in check. The restructuring of the food system along these lines will help to create the conditions for near-zero emissions on farms.

  • Rebuild the soil and retain the water

We have to take the soil seriously again. We need a massive global effort to build organic matter back into the soils, and bring back fertility. Decades of soil maltreatment with chemicals in many places, and mining of soils in others, have left soils exhausted. Healthy soils, rich in organic matter, can retain huge amounts of water, which will be needed to create resilience in the farming system, to deal with the climate and water crises that are already encroaching on us. Increasing organic matter in soils around the world will help to capture substantial amounts of the current excess CO2 in the atmosphere (see “Earth matters”, p. 9).

  • De-industrialise agriculture, save energy, and keep the people on the land

Small-scale family farming should become the cornerstone of food production again. By allowing the build-up of mega-industrial farm operations that produce commodities for the international market rather than food for people, we have created empty countrysides, overpopulated cities, and destroyed many livelihoods and cultures in the process. De-industrialising agriculture would also help to eliminate the tremendous waste of energy that the industrial farming system now produces.



  • Grow close by and cut the international trade

One principle of food sovereignty is to prioritise local markets over international trade. As we have seen, international trade in food, and its associated food processing industries and supermarket chains, are the food system’s chief contributors to the climate crisis. All of these can largely be cut out of the food chain if food production is reoriented towards local markets. Achieving this is probably the toughest fight of all, as so much corporate power is concentrated on keeping the trade system growing and expanding, and so many governments are happy to go along with this. But if we are serious about dealing with the climate crisis, this has to change.

  • Cut the meat economy and change to a healthier diet

Perhaps the most profound and destructive transformation that the industrial food system has brought upon us is in the livestock sector. What used to be an integral and sustainable part of rural livelihoods has become a mega-industrial meat factory system spread around the world, but controlled by a few. The international meat economy, which has grown fivefold in recent decades, is contributing to the climate crisis in an enormous way. It has also helped to create the obesity problem in rich countries, and destroyed – through subsidies and dumping – local meat production in poor countries. This has to stop, and consumption patterns, especially in rich countries, have to move away from meat. The world needs to return to a decentralised system of meat production and distribution, organised according to people’s needs. Markets that supply meat from smaller farms to local markets at fair prices need to be restored and reinvigorated, and international dumping has to stop.

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hunger and the impact to climate change.

The reason that land-use change is often lumped in with agriculture in the statistics on factors responsible for climate change is that much of it occurs through the conversion of forest or grassland to crop production or cattle raising. The FAO estimates that 90 per cent of deforestation is caused by agriculture, nearly all of it in developing countries.

Even so, farmers are conserving significant areas of forest. A recent study using detailed satellite imagery, carried out by the World Agroforestry Centre, shows that 46 per cent of the world’s farmland contains at least 10 per cent tree cover. The area revealed in this study is twice the size of the Amazon and shows that farmers are protecting and planting trees spontaneously. These trees already play an important role in protecting farmers against climate change and could help more, particularly as farmers in the tropics have a staggering 50,000 different tree species to choose from. When crops and livestock fail, trees often withstand drought conditions and allow people to hold over until the next season.

There are clearly other important reasons, apart from farming, why forests get cut down. Logging, mining, roads, urban sprawl and dams are also major causes of deforestation. So too is small-scale collection of fuel-wood, which is often driven by lack of access on the part of the poor to public sources of energy. In many countries, deforestation is camouflaged as agricultural development by companies who want to acquire land concessions for the timber. Palm oil and rubber companies are notorious for clearing virgin forest to get at the lumber, while not following through on promises to develop the land for agriculture.

That said, farmers do cut down forests to get at new farm lands. But we have to ask why they do so. Population pressures are only one part of the story. As the World Rainforest Movement has extensively documented, more often the problem is not a lack of agricultural land, but the concentration of land and/or resources in the hands of an elite, or the expulsion of communities to make way for development projects.

Deforestation tends to happen when communities lose control over their resources. Where deforestation occurs, there are usually local communities trying to stop it – especially communities of indigenous people. And where poor people clear forest for farmland, they were often pushed off of their former lands – and the odds are that they tried to resist the process, as witnessed by the backlog of court cases and petitions over land conflicts in countries such as Vietnam and China.

Moreover, those converting forests and grasslands to agriculture are not, in many cases, small farmers but transnational corporations (TNC), or large-scale farmers producing for TNCs. The expansion of oil-palm plantations in Indonesia’s rain forests or sugar-cane plantations in Brazil’s cerrado are two obvious examples. Indeed, it is hard to imagine how small farmers could cuase large-scale deforestation when, in many countries, they occupy only a small percentage of the agricultural land. In Latin America, in countries where such data is available, small farmers occupy only 3.5 per cent of the agricultural land in Ecuador, 8.5 per cent in Brazil and 5 per cent in Chile.In Colombia and Peru, where small farmers own most of the farms (82 per cent and 70 per cent, respectively, of the holdings), they occupy only a modest share of the farmed land (14 per cent and 6 per cent, respectively).

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