Category Archives: Regime Shifts

Mapping Coastal Eutrophication

Current industrial agricultural practices produce a tradeoff between agricultural production and the quality of coastal ecosystems, because agricultural fertilizers that increase crop yields lead to the creation of low oxygen hypoxic areas in areas which receive a lot of nutrient rich runoff.

The World Resources Institute and Virginia Institute of Marine Science, has updated Diaz et al’s recent map of coastal eutrophication. They identify 169 hypoxic areas, 233 areas of concern, and 13 systems in recovery.

Coastal Eutrophication WRI 2008

The WRI Earthtrends weblog writes about the project:

The map shows three types of eutrophic zones:

(1) Documented hypoxic areas – Areas with scientific evidence that hypoxia was caused, at least in part, by an overabundance of nitrogen and phosphorus. Hypoxic areas have oxygen levels low enough to inhibit the existence of marine life.

(2) Areas of concern – Systems that exhibit effects of eutrophication, including elevated nitrogen and phosphorus levels, elevated chlorophyll levels, harmful algal blooms, changes in the benthic community, damage to coral reefs, and fish kills. These systems are impaired by nutrients and are possibly at risk of developing hypoxia. Some of the systems may already be experiencing hypoxia, but lack conclusive scientific evidence of the condition.

(3) Systems in recovery – Areas that once exhibited low dissolved oxygen levels and hypoxia, but are now improving. For example, the Black Sea recovery is largely due to the economic collapse of Eastern Europe in the 1990s, which greatly reduced fertilizer use. Others, like Boston Harbor in the United States and the Mersey Estuary in the United Kingdom also have improved water quality resulting from better industrial and wastewater controls.

Given the state of global data, the actual number of eutrophic and hypoxic areas around the world is likely to be greater than the 415 listed here. The most under-represented region is Asia. Asia has relatively few documented eutrophic and hypoxic areas despite large increases in intensive farming methods, industrial development, and population growth over the past 20 years. Africa, South America, and the Caribbean also have few reliable sources of coastal water quality data.

A more detailed analysis of this data set will be available in February 2008 in a policy note entitled Eutrophication and Hypoxia in Coastal Areas: A Global Assessment of the State of Knowledge (a list of related publications can be found here.

How to deal with uncertainty in climate change economics

From the economist Martin L. Weitzman‘s website, a new draft paper On Modeling and Interpreting the Economics of Catastrophic Climate Change(pdf).  He proposes a method for including unlikely but extreme events (fat tails) in cost-benefit analyses, such as the uncertainty surrounding climate sensitivity.  Considering the possibility of such events can completely change the results of an analysis, and favour action as a type of catastrophe insurance.

Abstract: Using climate change as a prototype example, this paper analyzes the implications of structural uncertainty for the economics of low-probability high-impact catastrophes. The paper is an application of the idea that having an uncertain multiplicative parameter, which scales or amplifes exogenous shocks and is updated by Bayesian learning, induces a critical tail fattening of posterior-predictive distributions. These fattened tails can have very strong implications for situations (like climate change) where a catastrophe is theoretically possible because prior knowledge cannot place sufficiently narrow bounds on overall damages. The essence of the problem is the difficulty of learning extreme-impact tail behavior from finite data alone. At least potentially, the ináuence on cost-benefit analysis of fat-tailed uncertainty about climate change, coupled with extreme unsureness about high-temperature damages, can outweigh the influence of discounting or anything else.

The paper concludes:

In principle, what might be called the catastrophe-insurance aspect of such a fat-tailed unlimited-exposure situation, which can never be fully learned away, can dominate the social-discounting aspect, the pure-risk aspect, or the consumption-smoothing aspect. Even if this principle in and of itself does not provide an easy answer to questions about how much catastrophe insurance to buy (or even an easy answer in practical terms to the question of what exactly is catastrophe insurance buying for climate change or other applications), I believe it still might provide a useful way of framing the economic analysis of catastrophes.

Arctic sea ice: is it tipped yet?

RealClimate reports from the AGU about Arctic sea ice: is it tipped yet?

The summer of 2007 was apocalyptic for Arctic sea ice. The coverage and thickness of sea ice in the Arctic has been declining steadily over the past few decades, but this year the ice lost an area about the size of Texas, reaching its minimum on about the 16th of September. Arctic sea ice seems to me the best and more imminent example of a tipping point in the climate system. A series of talks aimed to explain the reason for the meltdown.

The disappearance of the ice was set up by warming surface waters and loss of the thicker multi-year ice in favor of thinner single-year ice. But the collapse of ice coverage this year was also something of a random event. This change was much more abrupt than the averaged results of the multiple IPCC AR4 models, but if you look at individual model runs, you can find sudden decreases in ice cover such as this. In the particular model run which looks most like 2007, the ice subsequently recovered somewhat, although never regaining the coverage before the meltback event.

So what is the implication of the meltback, the prognosis for the future? Has the tipping point tipped yet? When ice melts, it allows the surface ocean to begin absorbing sunlight, potentially locking in the ice-free condition. Instead of making his own prognosis, Overland allowed the audience to vote on it. The options were

* A The meltback is permanent
* B Ice coverage will partially recover but continue to decrease
* C The ice would recover to 1980’s levels but then continue to decline over the coming century

Options A and B had significant audience support, while only one brave soul voted for the most conservative option C. No one remarked that the “skeptic” possibility, that Arctic sea ice is not melting back at all, was not even offered or asked for. Climate scientists have moved beyond that.

For more coverage see Nature’s Great Beyond.

Eutrophication creates deformed frogs

Pieter T. J. Johnson et al have a new paper in PNAS Aquatic eutrophication promotes pathogenic infection in amphibians.

That shows how nutrient runoff from agriculture increase algal growth, which in turn leads to increases in snail populations that host parastites.  These parasites can then infect and deformed  frogs. What is particularly important is eutrophication, which is expected to increase with increased agricultural production, could enhance the spread of other diseases that harm people as well as wildlife.  The authors write:

Our results have broad applicability to other multihost parasites and their hosts. Recent increases in a variety of human and wildlife multihost parasites have been linked to eutrophication, including cholera, salmonid whirling disease, West Nile virus, coral diseases, and malaria.

Trematode parasites similar to Ribeiroia that use snails as intermediate hosts also infect humans, ranging from the nuisance, but relatively innocuous, cercarial dermatitis to the pathogenic schistosomiasis, which is estimated to afflict 200 million people across Africa and Asia.  If the life cycles of Schistosoma spp. are similarly affected by eutrophication, forecasted increases in agricultural nutrient applications in developing countries where schistosomiasis is endemic could hinder or inhibit efforts to control this disease.

For more see Wisconsin State Journal.

Partha Dasgupta on Lomborg’s muddled concreteness

Environmental economist Partha Dasgupt a reviews Cool It: The Skeptical Environmentalist’s Guide to Global Warming, by Bjorn Lomborg in Nature

Unfortunately, Lomborg’s thesis is built on a deep misconception of Earth’s system and of economics when applied to that system. The concentration of CO2 in the atmosphere is now 380 p.p.m., a figure that ice cores in Antarctica have revealed to be in excess of the maximum reached during the past 600,000 years. If there is one truth about Earth we all should know, it’s that the system is driven by interlocking, nonlinear processes running at different speeds. The transition to Lomborg’s recommended concentration of 560 p.p.m. would involve crossing an unknown number of tipping points (or separatrices) in the global climate system. We have no data on the consequences if Earth were to cross those tipping points. They could be good, or they could be disastrous. Even if we did have data, they would probably be of little value because nature’s processes are irreversible. One implication of the Earth system’s deep nonlinearities is that estimates of climatic parameters based on observations from the recent past are unreliable for making forecasts about the state of the world at CO2 concentrations of 560 p.p.m. or higher. Moreover, the nonlinearities mean that doing more of a bad deal (Kyoto) may well be very good.

These truths seem to escape Lomborg. His cost–benefit analysis involves only point estimates of variables (interpreted variously as ‘most likely’, ‘expected’, and so forth), implying that he believes we shouldn’t buy insurance against potentially enormous losses resulting from climate change. His concerns over the prevalence of malaria, undernutrition and HIV in today’s world show that he is an egalitarian. There is, then, an internal contradiction in his value system, because if you are averse to inequality you should also be averse to uncertainty.

The integrated assessment models of Earth’s system on which Lomborg builds his case are arbitrarily bounded on either side of his point estimates. It can be shown that if those bounds are removed (as they ought to be), even a small amount of uncertainty — when allied to only a moderate aversion to uncertainty — would imply that humanity should spend substantial amounts on insurance, even more than the 1–2% of world output that has been advocated. If the uncertainties are not small, standard cost–benefit analysis as applied to the economics of climate change becomes incoherent, even if those uncertainties are judged to be thin-tailed (gaussian, for example); this is because the analysis would say that no matter how much humanity chooses to invest in protecting Earth from passing through those later tipping points, we should invest still more.

Economics helps us to realize what we are able to say about matters that will reveal themselves only in the distant future. Simultaneously, it helps us to realize the limits of what we are able to say. That, too, is worth knowing, for limits on what we are able to say are not a reason for inaction. Lomborg’s seemingly persuasive economic calculations are a case of muddled concreteness.

Australian ecologist Tim Flannery makes some similar points in his review and concludes with the much stronger statement that:

By empathizing with those who are concerned about climate change and poverty, and trying to persuade them to divert their energies, Cool It is a stealth attack on humanity’s future.

Arctic sea ice at record low

In 2005 on Resilience Science, Line Gordon, wrote about recent research that we may have already passed tipping points in the Arctic.

NSIDC Arctic Sea Ice News Fall 2007 is providing weekly updates on the state of Arctic sea ice, which has reached record low coverage this year (the previous record low was in 2005).

Arctic Sea Ice

The figure shows daily ice extent for 2007, 2005 and to the 1979 to 2000 average.

Sandstorms and Land degradation in China

Gaoming Jiang, a professor at the Chinese Academy of Sciences’ Institute of Botany, writes about China’s failure to restore degraded arid land in a China Dialogue article Stopping the Sandstorms:

In Beijing, the weather forecast says that more sandstorms are on the way. The capital was hit by four sandstorms in March, and even Shanghai was recently smothered by dust clouds from the north. Television reports now describe these events as “sandy weather”, rather than “sandstorms”. But whatever you call them, they are becoming ever more frequent visitors to Beijing in springtime.

While everyone is cursing the weather, I find myself worrying: how many tonnes of soil are being lost? And how long will it be before there is nowhere in China for plants to take root? Academics argue to what extent these sandstorms are “imports” from Mongolia and the former Soviet Republics, or whether they are the “domestic” products of the arid deserts and damaged grasslands of China’s west. But either way, there is no denying the degree of environmental degradation in western China over the last three decades. Regardless of whether the capital’s weather comes from beyond its borders, China needs to put measures in place to restore the grasslands and reduce the risk of sandstorms.

Sixty billion yuan has been invested in projects to control the sandstorms that are hitting northeastern China. Tree-planting projects have also been running for 30 years across north China. But why haven’t they worked? And more importantly – what will?
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Climate change and Tipping Points in the Amazon

Most of the talks from a recent conference on Climate change and the fate of the Amazon at University of Oxford are available online as slides and podcasts. Some of the interesting points from the conference:

  • Intact forests may be more resistant to drought than climate-vegetation models usually assume (deep roots, large soil water reserves, hydraulic uplift)
  • The interaction of drought with forest fragmentation and fire ignition points can trigger tipping to savanna forest with less biodiversity and biomass.
  • Global demand for soybeans and biofuels could drive substantial land clearing.
  • Substantial opportuntities for land use change feedbacks exist in Amazonia. Climatic drying could allow the expansion of soy and sugarcane cultivation, which would feedback to stimulate further drying.
  • There is a need increase the resilience of the Amazon, because models estimate a non-trival chance of severe drought and forest dieback over the 21st century. Resilience can be enhanced by enhancing the recycling of water vapour that maintains mesic forests in the amazon.

David Oswald works on Amazonia forest resilience in my lab. He attended the conference and has these recommendations on the talks:

Carlos Nobre – Dr. Nobre is very well-known internationally and especially in Brazil. He is a climate scientist by training but is involved in the leadership of scientific research projects such as IGBP, CPTEC, and the LBA project. He alludes to the importance of Ecological Resilience and Stability in his talk, but more detail and a conceptual framework is required – (that is what I am working on).

Peter Cox – Dr. Cox is a well-known global climate modeller and first published a paper in 2000 about the “Dieback” of the Amazon. This was very controversial when it came out and inspired many people to look at this problem from different perspectives and also using different global climate models. The follow up work to the 2000 paper has similar results and unfortunately, one of the outcomes of the conference was that there is general concensus that increasing greenhouse gas emissions and the corresponding climate change could have very serious effects on the Amazon. Again, these research projects at this scale have a high degree of uncertainty, but the people presenting, who are all experts, came to similar conclusions. Check it out for yourself.

Chris Huntingford – Dr. Huntingford’s presentation was a follow up to Cox’s work, basically testing the hyothesis and strength of results.

Luiz Aragao – Dr. Aragao and his collaborators did some interesting work with remote sensing, similar to the type of approach I am taking. Very solid work.

Michael Keller – Dr. Keller is with the US Forest Service and has been involved with the LBA project in a leadership position since the early 90’s. He has a broad historical as well as sound scientific perspective on things.

Dan Neptad – Dr. Nepstad is extremely well known in Amazonian research and is at the Woods Hole Research center. He has done some very interesting work with water availability and ecosystem health in the Amazon and has designed some very cool experiments. Increasingly, his work is focused on the interaction between science and development policy in this region. His presentation speaks to that. He is a progressive thinker, and also very active on the ground in the Amazon.

Juan Carlos Riveros – Dr. Riveros gave a very interesting talk on conservation strategies in the Amazon. I was blown away by the extent of the research they have done and continue to do with respect to conservation strategies. They have done some very interesting spatial analytical work. Good for a geography-oriented person.

Diogenes Alves – Dr. Alves is an interesting person. By training, he is a computational mathematician. He has been involved extensively with the design and planning of the LBA project. His presentation outlined the epistemological framework they used and also some of the challenges they initally faced with the structuring of an international scientific research project that clearly was embedded in a complex social and economic situation. He alluded to Systems Theory in his talk, and that really appealed to me, so I am including this one for those that are interested in the links between Social Science and Natural Science and the practical realities one faces when doing this type of research.

Kevin Conrad – Mr. Conrad is with a group called the Rainforest Coalition. He presented a strategy for rainforest conservation based on using the Clean Development Mechanism of the Kyoto Protocol as a means of attaching economic value on the carbon market to rainforests that are preserved and not degraded. I did not understand in depth this strategy, but it seems that there are positive merits to this approach. I personally, am not 100% sold on exclusively using market solutions but I think that they do play an important role. For more detail you can check out his presentation and come to your own conclusions.

Dr. Yadvinder Malhi’s provides a summary of the conference. He draws out the key points and overall conclusions.

Resilience: Reflections part 3

My bridge to studying ecosystems started once I shifted to combine the functional and numerical response equations with others concerning other processes in order to make a population model, of interacting predator and prey. That is when, suddenly and unexpectedly, multi-stable states appeared. Lovely indeed. Great fun and a big surprise to me! A new landscape for exploration opened.

Non-linear forms of the functional responses (e.g. the Type 3 S-shaped response) and of reproduction responses (e.g. the Allee effect) interacted to create two stable equilibria for interacting populations, with an enclosed stability domain around one of them. It was the responses at low densities that were critical- that is where vertebrate predators have yet to learn to locate the prey easily, and where mates are too scarce to find each other easily. Once discovered, it seemed obvious that conditions for multi-stable states were inevitable. And that, being inevitable, there were huge consequences for theory and for practice.

Up to that time, a concentration on a single equilibrium and assumptions of global stability had made ecology, as well as economics, focus on near equilibrium behavior, and on fixed carrying capacity with a goal of minimizing variability. Command and control was the policy for managing fish, fowl, trees, herds, and freedom was unlimited to provide opportunity for people.

The multi-stable state reality, in contrast, opened an entirely different direction that focused on behavior far from equilibrium and on stability boundaries. High variability, not low variability, became an attribute necessary to maintain existence and learning. Surprise and inherent unpredictability was the inevitable consequence for ecological systems. Data and understanding at low densities, rare because they are all the more difficult to obtain, were more important than those at high-density. I used the word resilience to represent this latter kind of stability

Hence the useful measure of resilience was the size of stability domains, or, more meaningfully, the amount of disturbance a system can take before its controls shift to another set of variables and relationships that dominate another stability region. And the relevant focus is not on constancy but on variability. Not on statistically easy collection and analysis of data but statistically difficult and unfamiliar ones. That needs a different eye to see and a different theory to perceive consequences.

About that time, I was invited to write a 1973 review article for the Annual Review of Ecology and Systematics. I therefore decided to turn it into a review of the two different ways of perceiving stability and in so doing highlight the significance for theory and for practice. That required finding additional rare field data in the literature that demonstrated flips of populations from one level or state to another, as well as describing the recently discovered known non-linearities in the processes that caused or inhibited the phenomenon. That was a big job and I recall days when I thought it was all bunk, and days when I believed it was all real. I finished the paper on a “good” day, when all seemed pretty clear. By then I guess I was convinced. The causal, process evidence was excellent, though the field evidence concerning population flips, was only suggestive. Nevertheless the consequences for theory and management were enormous. It implied that uncertainty was inevitable. And that ecosystems, in an evolutionary time span, were momentary entities pausing in a flip to different states. As I’ll describe, it took about 30 years to confirm those conclusions for others.

This paper began to influence fields outside population/community ecology a bit – anthropology, political science, systems science first, then, later, ecosystem science. It became the theoretical foundation for active adaptive ecosystem management. But it was largely ignored or opposed by practitioners in the central body of ecology. What followed was the typical and necessary skepticism released by new ideas, that I’ll describe briefly here because it is such a common foundation for developing science.

One early ecological response to the paper was by Sousa and Connell (1985). They asked the good question “was there empirical evidence for multi-stable states?”. They attempted to answer by analyzing published data on time series of population changes of organisms to see if the variance suggested multi-stable behavior. They found no such evidence. This so reinforced the dominant population ecology single equilibrium paradigm, that the resilience concept was stopped dead, in that area of science.

It seemed to be an example of evidence that refuted this new theory. But their evidence was inappropriate and the theory was not! In fact, their evidence, as is often the case, was really a model, incomplete because the collators unconsciously used an inappropriate model for choosing data that were incomplete.

There are two problems with their analysis:

  1. They did not ask any process question (are there common non-linear mechanisms that can produce the behavior?). That is where the good new hard evidence that I had discovered lay.
  2. They rightly saw the need for long time series data on populations that had high resolution. As population/community ecologists of tradition, however, their view of time was a human view- decades were seen as being long. That view is reinforced by a “quadrat” mentality. Not only small in time, but small in spatial scale; and a theory limited to linear interactions between individuals in single species populations or between two species populations, all functioning at the same speed (e.g. predator/prey, competitors). It represents the dangers caused by inferring that “microcosm” thought and experiments have anything to contribute to the multiscale functioning of ecosystems. Steve Carpenter has a perceptive critique of that tendency (Carpenter, 1996).

The multi-stable behavior can only be interpreted within the context of at least three but, as suggested in the Panarchy paper/chapter, probably not more than five variables. These variables need to differ qualitatively in speed from each other. It is therefore inherently ecosystemic. It is the slow variables that determine how many years of data are needed for their kind of test. None of their examples had anywhere near the duration of temporal data needed.

As an example: The available 45 years of budworm population changes they analyzed seemed long to Sousa and Connell and to all those conditioned by single variable behavior and linear thinking of the times. But the relevant time scale for the multi-equilibrium behavior of budworm is set by their hosts, the trees or the slow variable. What is needed for their tests was yearly budworm data (the fast variable) over several generations of trees (the slow variable), i.e. perhaps one and a half centuries – not 45 years. The normal boom and bust cycle is 40-60 years

It has since taken 25 years of study of different ecosystems to develop data for appropriate tests. Examples include those using paleo-ecological data covering centuries at high resolution, the deep and shallow lake studies and experiments of Carpenter (Carpenter 2000) in the United States and of Marten Scheffer, in Europe (Scheffer et al. 1993), the experimental manipulations of mammalian predator and prey systems in Australia and Africa by Tony Sinclair (Sinclair et al. 1990), and a variety of studies of specific ecosystems- sea urchin, coral reef etc. Terry Hughes and his colleagues’ works on coral reefs stand out as examples. Carpenter’s important summary paper makes the point (Carpenter, 2000). Multi-stable states are real and of great importance, although they are difficult to demonstrate. Surprise, uncertainty and unpredictability are the inevitable result. Command and control management temporarily hides the costs, but the ultimate cost of surprises produced by managing systems that ignore multi-stable properties is too great. Active adaptive management is the only alternative management response possible. Steve Carpenter and Buz (W.A.) Brock – a great ecosystems scientist together with a wonderful ”non-linear” economist- show why in a classic paper where a minimal model of a watershed, farming styles, of regional monitoring and regional decision regarding phosphate control, encounter the surprises created as a consequence of a multi-stable state (Carpenter, Brock, and Hanson, 1999).

References:

Carpenter, Stephen R. 1996. Microcosm experiments have limited relevance for community and ecosystem ecology. Ecology 77 (3) : 677-690.

Carpenter, S.R. 2000. Alternate states of ecosystems. Evidence and its implications for environmental decisions. In, M.C.Press, N.Huntley and S. Levin. (eds). Ecology: Achievement and Challenge, Blackwell, London.

Carpenter, S.R., Brock, W.A., Hanson, P.C., 1999. Ecological and social dynamics in simple models of ecosystem management. Conservation Ecology 3(2), 4. URL: http://www.consecol.org/vol3/iss2/art4

Scheffer, M., S.H. Hopsper, M-L. Meijer, B.Moss and E. Jeppesen. 1993. Alternative equilibria in shallow lakes. Trends in Ecol. & Evol. 8 (8): 275- 279.

Sinclair, A.R.E. , P.D. Olsen, and T.D. Redhead. Can predators regulate small mammal populations? Evidence from mouse outbreaks in Australia. Oikos 59: 382-392.

Sousa, W.P. and J.H. Connell. 1985. Further comments on the evidence for multiple stable points in natural communities. American Naturalist 125, 612-615.

      Hidden Ecological Functions and Ecological Hysteresis

      BatfishThe paper by coral reef researchers Bellwood, Hughes, & Hoey, Sleeping functional group drives coral-reef recovery in Current Biology (2006 16(24):2434 -9) shows that hidden ecological functions can be critical for ecological restoration and provides further evidence for the importance of hysteresis in ecological regime shifts.

      The researchers were examining the frequently observed shift of coral reefs from being dominated coral to macroalgae. This change is often due to the overharvesting of herbivorous fishes, particularly parrotfishes and surgeonfishes, that maintain the coral regime. They showed that a shift to the marcoalgae dominated regime on the Australian Great Barrier Reef was reversed not by parrotfishes or surgeonfishes, but rather by a species of batfish, Platax pinnatus, which is relatively rare on the Great Barrier Reef, and was thought to feed only on invertebrates.

      Their finding suggests three things:

      1. that conserving ecosystem functioning is important for both for the maintenance and recovery of ecosystems,
      2. that successful functional conservation requires that we need to greatly increase our functional understanding of ecosystems, and
      3. that research into ecosystem functioning should examine function in different ecological contexts.

      Interestingly, this research finding is similar to that of common property researchers who have discovered that many local resource management institutions contain “hidden” resources management practices, that are only activated during special environmental conditions – for example a fishery may have alternative property rights emerge during periods low fish abundance.

      Press coverage of this research can be found in a press release from James Cook University, the New Scientist, and the Washington Post.