Category Archives: Ideas

Hydrological impact of biofuels

R. Dominguez-Faus and others analyze the impact of different biofuels on water in the USA in their article in Envir. Science and Technology, The Water Footprint of Biofuels: A Drink or Drive Issue? (doi:10.1021/es802162x).  The figure below, from the paper, shows the substantial ecological requirements (and variation) among biofuels.

Figure 1. Evapotranspiration, irrigation, and land requirements to produce 1 L of ethanol (Le) in the U.S. from different crops.

Figure 1. Evapotranspiration, irrigation, and land requirements to produce 1 L of ethanol (Le) in the U.S. from different crops.

They write:

The current and ongoing increase in biofuel production could result in a significant increase in demand for water to irrigate fuel crops, which could worsen local and regional water shortages. A substantial increase in water pollution by fertilizers and pesticides is also likely, with the potential to exacerbate eutrophication and hypoxia in inland waters and coastal areas including Chesapeake Bay and the Gulf of Mexico. This in turn would cause undue financial hardship on the fishing industry as well as negative impacts to these vital, biodiversity-rich, ecosystems. Such threats to water availability and water quality on local and national scales represent a major obstacle to sustainable biofuel production and will require careful assessment of crop selection and management options. It is important to recognize that certain crops such as switchgrass and other lignocelluosic options deliver more potential biofuel energy with lower requirements for agricultural land, agrichemicals, and water.

Climatic factors such as frequency of droughts and floods are beyond human control, but as the wide range of estimated nutrients discharged to surface waters shows, clearly some important variables are within our control. These include crop selection, tillage methods, and location. As more biofuel production is integrated into the agriculture sector it will be important to adopt land-use practices that efficiently utilize nutrients and minimize erosion, such as co-cropping winter grains and summer biomass crops. These land use choices should also focus on establishing riparian buffers and filter strips to serve a dual purpose in erosion control and biomass production. Similarly, a CRP-like program should be considered to promote cellulosic biofuel crop planting in marginal lands to prevent excess erosion and runoff while allowing producers to benefit from historically high commodity prices. CRP-like payments would then help to balance societal goals with ecological benefits and provide financial viability for the farmers making the land use choices. Finally, increasing charges for irrigation water for biofuel crops to market rates should be considered to promote fuel crop agriculture in areas where rainfall can supply the majority of the water requirements and to reflect the true value of water resources in the price of biofuels. Policies and programs should be coordinated to avoid the current situation where some efforts (ethanol subsidies, mandates) bid against other programs (CRP) though both are funded by taxpayers with the common goal of environmental protection.

Peatlands as complex adaptive systems

Shifting states. (Left) Hummock-hollow pattern at Rygmossen, a small raised bog near Uppsala, Sweden. (Right) "Ladder" system of ridges and pools, Inverewe Bogs, Scotland. Persistent environmental change, such as a long-term increase in climate wetness, can trigger a shift from one such peatland type to another.

Shifting states. (Left) Hummock-hollow pattern at Rygmossen, a small raised bog near Uppsala, Sweden. (Right) "Ladder" system of ridges and pools, Inverewe Bogs, Scotland. Persistent environmental change, such as a long-term increase in climate wetness, can trigger a shift from one such peatland type to another.

In a Perspective in Science, Nancy Dise reviews how the response of peatlands to global change will be complex (doi:10.1126/science.1174268). She writes:

Research from a variety of areas and approaches is converging upon the concept of peatlands as complex adaptive systems: self-regulating to some degree, but capable of rapid change and reorganization in response to internal developmental changes or to external forcing (4). It has long been known, for instance, that the surface of a peatland can rise and fall, sometimes dramatically, in response to rainfall or mild drought, while maintaining a fairly constant water level relative to the surface. This “Mooratmung” (“bog-breathing”) is related to the sponge-like nature of Sphagnum, which can adsorb water and trap gases. Recent studies have shown that the carbon balance of peatlands can in turn be surprisingly resilient to perturbations, even fairly severe ones. For example, subjecting peat cores (5) or a peatland field site (6) to a water table drawdown similar to a prolonged drought initially led to a respiration-driven loss of soil carbon. But both carbon loss and subsidence (6) lowered the peat surface, decreasing its height above the water table, and effectively shifted the system back toward its starting state. Conversely, a rising water table stimulated growth of Sphagnum and other vegetation, which increased carbon accumulation, raised the surface of the peat and, in effect, lowered the local water table (5). Thus, an environmental perturbation may trigger an initial gain or loss of carbon, but recovery in the direction of the initial state can moderate the impact.

Long-term global changes—particularly warming, drought, and elevated nitrogen deposition—are likely to ultimately induce shifts in some existing peat-forming areas to new ecosystems such as grassland or shrubland (10, 11), and the increase in biomass from vascular plants could in part compensate for carbon losses from soil oxidation during the transition. However, even if some net carbon accumulation returns, the gains are short-lived: The key peatland quality of slowly removing and storing carbon for hundreds or thousands of years is lost.

Considering peatlands as complex adaptive systems characterized by quasistable equilibrium states—resilient to change at some level of perturbation but shifting to new states at higher levels of disturbance—provides a meaningful framework for understanding and modeling their response to environmental change. Ignoring the strong feedbacks inherent in peatlands may lead to substantial under- or overestimates of their response to global change. The challenge is to forecast both the future environmental conditions that peatlands will experience and the internal feedbacks and state changes that may be triggered by these conditions. To meet this challenge it is vital to continue and expand long-term monitoring networks to characterize the present, paleo-environment research to reconstruct the past, and manipulation experiments in the field and laboratory to build our understanding of these unique and valuable ecosystems.

Oil Prices and the Financial Crisis

The Financial Times suggests that the IEA agrees with Herman Daly (at least a little bit), in  Did oil cause the latest recession? IEA weighs into the debate:

A feature in the draft executive summary of the IEA’s World Energy Outlook, which will be published tomorrow, revisits this argument and comes to a rather worrying conclusion.

It starts out keeping in line with the prevailing view: the run-up in oil prices from 2003 to mid-2008 played “an important, albeit secondary” role in the global economic downturn that took hold last year. Higher oil prices made oil-importing countries more vulnerable to the financial crisis, it says.

The feature concludes, however, on a somewhat stronger note.

The IEA points out that it had warned in 2006 that the effect of high oil prices from the preceding four years had not yet worked their way through the world economy, and that further increases in prices would “pose a significant threat to the world economy, by causing a worsening of current account imbalances and by triggering abrupt exchange rate realignments, a rise in interest rates and a slump in house and other asset prices”.

Transition Towns and Resilience Thinking

straplineThe concept of resilience appears to be really spreading.  One interesting group of people attempting to build resilience in specific communities is the Transition town movement. A global network of communities each of which is attempting to build their resilience to climate change and peak oil while addressing the question:

“for all those aspects of life that this community needs in order to sustain itself and thrive, how do we significantly increase resilience (to mitigate the effects of Peak Oil) and drastically reduce carbon emissions (to mitigate the effects of Climate Change)?”

Rob Hopkins is co-founder of the Transition Network, which connects together the Transition Town movement.  He recently wrote an article about Resilience Thinking and transition for Resurgence magazine.  The definition of resilience from the RA’s wesbsite  starts his article Why ‘resilience thinking’ is a crucial missing piece of the climate-change jigsaw and why resilience is a more useful concept than sustainability

Resilience; “the capacity of a system to absorb disturbance and reorganise while undergoing change, so as to retain essentially the same function, structure, identity and feedbacks”

In July 2009, UK Secretary of State for Energy and Climate Change Ed Miliband unveiled the government’s UK Low Carbon Transition Plan, a bold and powerful statement of intent for a low-carbon economy in the UK. It stated that by 2020 there would be a five-fold increase in wind generation, feed-in tariffs for domestic energy generation, and an unprecedented scheme to retrofit every house in the country for energy efficiency. In view of the extraordinary scale of the challenge presented by climate change, I hesitate to criticise steps in the right direction taken by government. There is, though, a key flaw in the document, which also appears in much of the wider societal thinking about climate change. This flaw is the attempt to address the issue of climate change without also addressing a second, equally important issue: that of resilience.

The term ‘resilience’ is appearing more frequently in discussions about environmental concerns, and it has a strong claim to actually being a more useful concept than that of sustainability. Sustainability and its oxymoronic offspring sustainable development are commonly held to be a sufficient response to the scale of the climate challenge we face: to reduce the inputs at one end of the globalised economic growth model (energy, resources, and so on) while reducing the outputs at the other end (pollution, carbon emissions, etc.). However, responses to climate change that do not also address the imminent, or quite possibly already passed, peak in world oil production do not adequately address the nature of the challenge we face.

Resilience thinking can inspire a degree of creative thinking that might actually take us closer to solutions that will succeed in the longer term. Resilient solutions to climate change might include community-owned energy companies that install renewable energy systems in such a way as to generate revenue to resource the wider relocalisation process; the building of highly energy-efficient homes that use mainly local materials (clay, straw, hemp), thereby stimulating a range of potential local businesses and industries; the installation of a range of urban food production models; and the re-linking of farmers with their local markets. By seeing resilience as a key ingredient of the economic strategies that will enable communities to thrive beyond the current economic turmoil the world is seeing, huge creativity, reskilling and entrepreneurship are unleashed.

The Transition Movement is a rapidly growing, ‘viral’ movement, which began in Ireland and is now under way in thousands of communities around the world. Its fundamental premise is that a response to climate change and peak oil will require action globally, nationally, and at the scale of local government, but it also needs vibrant communities driving the process, making unelectable policies electable, creating the groundswell for practical change at the local level.

It explores the practicalities of building resilience across all aspects of daily life. It catalyses communities to ask, “How are we going to significantly rebuild resilience in response to peak oil and drastically reduce carbon emissions in response to climate change?”

By putting resilience alongside the need to reduce carbon emissions, it is catalysing a broad range of initiatives, from Community Supported Agriculture and garden-share schemes to local food directories and new Farmers’ Markets. Some places, such as Lewes and Totnes, have set up their own energy companies, in order to resource the installation of renewable energy. The Lewes Pound, the local currency that can only be spent in Lewes, recently expanded with the issuing of new £5, £10 and £20 notes. Stroud and Brixton are set to do the same soon.

Reviewing Critical Transitions

transcoverEnvironmental historian, John R. McNeill, reviews Marten Scheffer‘s new book on resilience – Critical Transitions in Nature and Society. In the American Scientist he writes:

Like many before him, Marten Scheffer is impressed with parallels between social systems and natural systems. Moreover, he is convinced that problems confronting the human race require something more integrated than the fragmentary knowledge of the various academic disciplines. In short, he seeks to span the famous “two cultures” and to take a long stride toward consilience. Coming from a background in limnology and aquatic ecology, Scheffer is inevitably more at home in some arenas of knowledge than others, and his new book, Critical Transitions in Nature and Society, is mainly about the critical transitions in nature that are of interest to society. An example with which he begins the book is typical: the transformation of the Western Sahara into desert about 5,500 years ago as a result of initially small climate change that built on itself because the drier climate reduced vegetation, thereby heightening albedo.

Part of Scheffer’s aim is to contribute to the study of how well the theory of system dynamics corresponds to real life, in the behavior both of nature and of society. “If we are able to pin down the mechanisms at work,” he says, “this may eventually open up the possibility of predicting, preventing, or catalyzing big shifts in nature and society.” To be able to do so is a long-standing human ambition, which has been given fullest rein in political regimes that have seen utopia just over the horizon and have aimed to get there as soon as possible. In the abstract, such ambition seems laudable. In practice, it has led to many regrettable “big shifts” in nature and society, such as those undertaken in the headiest days of the Soviet Union or Mao Zedong’s rule in China. To date, those most keen on provoking “big shifts” have known far too little, and perhaps cared too little as well, about the possible outcomes of their actions. When results did not conform closely enough to their hopes, they used their powers to try to force society and nature into preferred channels, which led to gulags and environmental disasters. When trying to catalyze big shifts in nature and society, one must really know what one is doing—and that is very, very hard to do.

So Scheffer seems more cheerful about the future of the Social-Eco-Earth-System at the end of writing his book than I am after reading it. But his premise—that hope lies with integrated eco-social science rather than our traditional isolated silos of knowledge—is surely correct. Perhaps we are on the edge of a happy tipping point after which science enters a state in which depth is not unduly esteemed over breadth, in which integrated study of complex systems becomes the norm, in which our insight into real-world eco-social systems grows and grows to formerly unimaginable levels. If so, Scheffer may be right to be optimistic. But there are some powerful attractors working against it.

Resilience as an operating system for sustainability in the anthropocene

Chris Turner, author of Geography of Hope: A Tour of the World We Need, writing in the Walrus about the Anthropocene and the coral reef crisis in his long article Age of Breathing Underwater:

I first heard tell of “resilience” — not as a simple descriptive term but as the cornerstone of an entire ecological philosophy — just a couple of days before I met Charlie Veron on the pages of Melbourne’s most respected newspaper. I was onstage for the opening session of the Alfred Deakin Innovation Lectures in an auditorium at the University of Ballarat at the time. The evening had begun with a literal lament — a grieving folk song performed by an aboriginal musician. I’d then presented a slide show of what I considered to be the rough contours of an Anthropocene map of hope, after which a gentleman I’d just met, a research fellow at Australia’s prestigious Commonwealth Scientific and Industrial Research Organisation named Brian Walker, placed my work in the broader context of resilience theory.

I had to follow Veron all the way to the edge of the abyss his research had uncovered before I could come back around to resilience. The concept, it turns out, emerged from the research of a Canadian-born academic named Buzz Holling at the University of Florida, and has since been expanded by a global research network called the Resilience Alliance. “Ecosystem resilience” — this in the Resilience Alliance website’s definition — “is the capacity of an ecosystem to tolerate disturbance without collapsing into a qualitatively different state that is controlled by a different set of processes. A resilient ecosystem can withstand shocks and rebuild itself when necessary.” It’s a concept I encountered repeatedly in my conversations with reef researchers.

…This points to the broader implications of the resilience concept — the stuff Brian Walker likes to talk about. He and his colleagues in the Resilience Alliance often refer to their field of study as “social-ecological resilience,” suggesting that people are as essential to the process as reefs or any other ecosystem, and that real resilience is created in the complex, unpredictable interplay between systems. “With resilience,” Walker told me, “not only do we acknowledge uncertainty, but we kind of embrace uncertainty. And we try to say that the minute you get too certain, as if you know what the answer is, you’re likely to come unstuck. You need slack in the system. You need to have the messiness that enables self-organization in the system in ways that are not predictable. The best goal is to try to build a general resilience. Things like having strong connectivity, but also some modularity in the system so it’s not all highly connected everywhere. And lots of diversity.”

Resilience, then, embraces change as the natural state of being on earth. It values adaptation over stasis, diffuse systems over centralized ones, loosely interconnected webs over strict hierarchies. If the Anthropocene is the ecological base condition of twenty-first-century life and sustainability is the goal, or bottom line, of a human society within that chaotic ecology, then resilience might be best understood as the operating system Paul Hawken was on about — one with an architecture that encourages sustainability in this rapidly changing epoch.

This new operating system will, by necessity, be comfortable with loss. There is, after all, much to be gained from epochal, transformative change. In the midst of chaos and devastation on the scale of a world war, for example, we might discover how to breathe underwater.

Uncertainty and climate change

Australian Economist, John Quiggin points out that uncertainty should increase intensity of climate change action.  He writes

…it’s a straightforward implication of standard economic analysis that the more uncertainty is the rate of climate change the stronger is the optimal policy response. That’s because, in the economic jargon, the damage function is convex. To explain this, think about the central IPCC projection of a 3.5 degrees increase in global mean temperature, which would imply significant but moderate economic damage (maybe a long-run loss of 5-10 per cent of GDP, depending on how you value ecosystem effects). In the most optimistic case, that might be totally wrong – there might be no warming and no damage. But precisely because this is a central projection it implies an equal probability that the warming will be 7 degrees, which would be utterly catastrophic. So, a calculation that takes account of uncertainty implies greater expected losses from inaction and therefore a stronger case for action. This is partly offset by the fact that we will learn more over time, so an optimal plan may involve an initial period where the reduction in emissions is slower, but there is an investment in capacity to reduce emissions quickly if the news is bad. This is why its important to get an emissions trading scheme in place, with details that can be adjusted later, rather than to argue too much about getting the short term parts of the policy exactly right.

Anyway, back to my main point. The huge scientific uncertainty about the cost of inaction has obscured a surprisingly strong economic consensus about the economic cost of stabilising global CO2 concentrations at the levels currently being debated by national governments, that is, in the range 450-550 ppm. The typical estimate of costs is 2 per cent of global income, plus or minus 2 per cent. There are no credible estimates above 5 per cent, and I don’t think any serious economist believes in a value below zero (that is, a claim that we could eliminate most CO2 emissions using only ‘no regrets’ policies).

For anyone who, like me, is confident that the expected costs of doing nothing about emissions, relative to stabilisation, are well above 5 per cent of global income that makes the basic choice an easy one.

Minsky’s Financial Instability Hypothesis

Historian Stephen Mihm writes in the Boston Review on Hyman Minsky‘s work on the unstable dynamics of capitalism in Why capitalism fails:

Minsky called his idea the “Financial Instability Hypothesis.” In the wake of a depression, he noted, financial institutions are extraordinarily conservative, as are businesses. With the borrowers and the lenders who fuel the economy all steering clear of high-risk deals, things go smoothly: loans are almost always paid on time, businesses generally succeed, and everyone does well. That success, however, inevitably encourages borrowers and lenders to take on more risk in the reasonable hope of making more money. As Minsky observed, “Success breeds a disregard of the possibility of failure.”

As people forget that failure is a possibility, a “euphoric economy” eventually develops, fueled by the rise of far riskier borrowers – what he called speculative borrowers, those whose income would cover interest payments but not the principal; and those he called “Ponzi borrowers,” those whose income could cover neither, and could only pay their bills by borrowing still further. As these latter categories grew, the overall economy would shift from a conservative but profitable environment to a much more freewheeling system dominated by players whose survival depended not on sound business plans, but on borrowed money and freely available credit.

Once that kind of economy had developed, any panic could wreck the market. The failure of a single firm, for example, or the revelation of a staggering fraud could trigger fear and a sudden, economy-wide attempt to shed debt. This watershed moment – what was later dubbed the “Minsky moment” – would create an environment deeply inhospitable to all borrowers. The speculators and Ponzi borrowers would collapse first, as they lost access to the credit they needed to survive. Even the more stable players might find themselves unable to pay their debt without selling off assets; their forced sales would send asset prices spiraling downward, and inevitably, the entire rickety financial edifice would start to collapse. Businesses would falter, and the crisis would spill over to the “real” economy that depended on the now-collapsing financial system.

It sounds very similar to Holling’s adaptive cycle and the pathology of natural resource management.

Planetary Boundaries

nature-climate-graphic-225A number of resilience researchers, and many others, have proposed the concept of planetary boundaries in a new paper A safe operating space for humanity in Nature (doi:10.1038/461472a).

Johan Rockstrom and others propose nine planetary boundaries, beyond which the functioning of the earth system will fundamentally change.  They argue that we have crossed the climate, nitrogen and extinction boundaries, and need to change the course of our civilization to move back into  conditions which provide a safety for human civilization.

Nature has a special feature on Planetary Boundaries.  It has also published seven independent essays by experts who reflect upon each of the defined boundary (two of the nine were not defined due to a lack of information), and their blog Climate Feedback is also hosting a discussion of the article.

Science journalist, Carl Zimmer has written a good article about the paper and concept on Yale’s Environment 360.

The Stockholm Resilience Centre provides links to the full paper, and supporting information, as well as a number of videos explaining the concept.

New measures of national well-being are moving towards mainstream

Alternative measures of national well-being are moving further towards the mainstream.

Economist Joseph Stiglitz writes in the Financial Times about a report, commissoned by the President of France he lead.   President Sarkozy, established the International Commission on the Measurement of Economic Performance and Social Progress, which produced a report on the measurement of economic performance and social progress.  Stiglitz writes about the report in the Financial Times article – Towards a better measure of well-being.

National income statistics such as GDP and gross national product were originally intended as a measure of market economic activity, including the public sector. But they have increasingly been thought of as measures of societal well-being, which they are not. Of course, good statisticians have warned against this error. Much economic activity occurs within the home – and this can contribute to individual well-being as much as, or more than, market production.

There are concerns, too, that a focus on the material aspects of GDP may be especially inappropriate as the world faces the crisis of global warming. Should we “punish” a country – in terms of our measure of performance – if it decides to take some of the fruits of the increase in productivity from the advancement of knowledge in the form of leisure, rather than just consuming more and more goods?

What we measure affects what we do. If we have the wrong metrics, we will strive for the wrong things. In the quest to increase GDP, we may end up with a society in which most citizens have become worse off. We care, moreover, not just for how well off we are today but how well off we will be in the future. If we are borrowing unsustainably from this future, we should want to know.

Flawed statistics may also lead us to make incorrect inferences. In the years preceding the crisis, many in Europe, focusing on America’s higher rates of GDP growth, were drawn to the US model. Had they focused on metrics such as median income – providing a better picture of what is happening to most Americans – or made corrections for the increased indebtedness of households and the country as a whole, their enthusiasm might have been more muted.

… Advances in research across a number of disciplines enable us now to develop broader, more encompassing measures of well-being. Such measures recognise that unemployment has an effect that goes well beyond the loss of income to which it gives rise. Health, education, security and social connectedness all are important to quality of life – but are not adequately reflected in GDP.

Newsweek reports:

The report recommends shifting economic emphasis from simply the production of goods to a broader measure of overall well-being, which would include the benefits of things like health, education, and security. It calls for greater focus on the effects on income inequality, as well as new ways to measure the economic impact of sustainability (climate change specialists like Nicolas Stern are members), and recommended ways to include the value of wealth to be passed on to the next generation into today’s economic conversation. What it didn’t do is come up with a quick and easy new way to tabulate a new measure of wellbeing. Some of the necessary yardsticks already exist; others still need to be invented.

Still, Sarkozy said he plans to shop the report all over the world. “France will open the debate on this report’s conclusions everywhere. It will put it on the agenda of every international conference, every meeting, every discussion where building a new economic, social, and ecological order is the objective,” he told the Sorbonne crowd. “France will fight for every international organization to modify their statistical systems by following the commission’s recommendations. It will propose to its European partners that Europe set the example by putting them into action. [France] will adapt its own statistical machinery in consequence,” he promised. Even the commission’s rapporteur admitted he wasn’t expecting Sarkozy’s strong reaction.