Category Archives: Ideas

How slow change increased California’s fire risk

California firesThe Christian Science Monitor article California’s age of megafires describes how California’s fire risk has been increased by slow changes in fire suppression (but probably not in California), climate change, longer fire season, and house construction in the wildland-urban interface:

Megafires, also called “siege fires,” are the increasingly frequent blazes that burn 500,000 acres or more – 10 times the size of the average forest fire of 20 years ago. One of the current wildfires is the sixth biggest in California ever, in terms of acreage burned, according to state figures and news reports.The trend to more superhot fires, experts say, has been driven by a century-long policy of the US Forest Service to stop wildfires as quickly as possible. The unintentional consequence was to halt the natural eradication of underbrush, now the primary fuel for megafires.

Three other factors contribute to the trend, they add. First is climate change marked by a 1-degree F. rise in average yearly temperature across the West. Second is a fire season that on average is 78 days longer than in the late 1980s. Third is increased building of homes and other structures in wooded areas.

“We are increasingly building our homes … in fire-prone ecosystems,” says Dominik Kulakowski, adjunct professor of biology at Clark University Graduate School of Geography in Worcester, Mass. Doing that “in many of the forests of the Western US … is like building homes on the side of an active volcano.”

In California, where population growth has averaged more than 600,000 a year for at least a decade, housing has pushed into such areas.

“What once was open space is now residential homes providing fuel to make fires burn with greater intensity,” says Terry McHale of the California Department of Forestry firefighters union. “With so much dryness, so many communities to catch fire, so many fronts to fight, it becomes an almost incredible job.”

Water in the American West: Learning from Crisis

Jon Gertner writes in The Future Is Drying Up a New York Times Magazine about Water in the American West. The articles is discusses how increases in population and decreases in precipitation are reorganizing the US inland west. It includes some insightful comments from Roger Pulwarty, a climatologist at NOAA who looks at adaptive solutions to drought. He sounds a bit like Emory University ecological management scientist Lance Gunderson:

You don’t need to know all the numbers of the future exactly,” Pulwarty told me over lunch in a local Vietnamese restaurant. “You just need to know that we’re drying. And so the argument over whether it’s 15 percent drier or 20 percent drier? It’s irrelevant. Because in the long run, that decrease, accumulated over time, is going to dry out the system.” Pulwarty asked if I knew the projections for what it would take to refill Lake Powell, which is at about 50 percent of capacity. Twenty years of average flow on the Colorado River, he told me. “Good luck,” he said. “Even in normal conditions we don’t get 20 years of average flow. People are calling for more storage on the system, but if you can’t fill the reservoirs you have, I don’t know how more storage, or more dams, is going to help you. One has to ask if the normal strategies that we have are actually viable anymore.”

Pulwarty is convinced that the economic impacts could be profound. The worst outcome, he suggested, would be mass migrations out of the region, along with bitter interstate court battles over the dwindling water supplies. But well before that, if too much water is siphoned from agriculture, farm towns and ranch towns will wither. Meanwhile, Colorado’s largest industry, tourism, might collapse if river flows became a trickle during summertime. Already, warmer temperatures have brought on an outbreak of pine beetles that are destroying pine forests; Pulwarty wonders how many tourists will want to visit a state full of dead trees. “A crisis is an interesting thing,” he said. In his view, a crisis is a point in a story, a moment in a narrative, that presents an opportunity for characters to think their way through a problem. A catastrophe, on the other hand, is something different: it is one of several possible outcomes that follow from a crisis. “We’re at the point of crisis on the Colorado,” Pulwarty concluded. “And it’s at this point that we decide, O.K., which way are we going to go?”

For some photos see NASA, and a graph of the water levels in Lake Mead showing the longterm decline in water storage.

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.

Scholarly networks on resilience, vulnerability and adaptation – update

Marco Janssen has updated his 2006 analysis of scholary networks in global change resilience, vulnerability and adaptation research. For his new paper in Ecology and Society (Janssen 2007) Janssen added more than 1000 new publications to the database, to analyze a total of 3399 publications from between 1967 and 2007. His analysis shows both rapid increase in the publications in the field, as well as increased integration of the three knowledge domains

Janssen mapped the co-author network of the almost 7000 unique authors in the data set. He selected the 16 most productive authors with a minimum of 15 papers. Both sets make up the set of 17 authors who are very productive and/or collaborative. Next, we determined all co-authors for those 17 authors, but kept only the 69 authors who had published a minimum of six papers.

figure 2

The figure above shows the most productive and best connected authors with the strongest co-authorship relations. Circles denote author nodes, and are labeled by the author’s last name and initials. Legend: Node – author; Node area size—# of publications; Node area color—# of unique co-authors.

Also, interestingly, three of the journals that contain the most articles in this field were newly founded in the past decade: Global Environmental Change, Ecology and Society, and Ecosystems. Ecology and Society is the most journal with the most papers in the resilience domain and the 4th greatest number of citation.

Key works that are heavily cited across research communities are:

Burton, I., R. W. Kates, and G. F. White. 1978. The environment as hazard. Oxford University Press, New York, New York, USA.

Holling, C. S. 1973. Resilience and stability of ecological systems. Annual Review of Ecology and Systematics 4:1–23.

Seasonal Rain Floods the Sahel

From NASA Earth Observer Seasonal Rain Floods the Sahel:

The Sahel region gets most of its rainfall between June and September when the band of near-perpetual thunderstorms that hover around the Equator shifts north. In 2007, the final months of the rainy season brought unusually heavy rainfall to East, Middle, and West Africa, causing floods in river basins from the Atlantic to the Indian Ocean coasts of the continent.

sahel flooding

This image illustrates how extensive the extreme rainfall was. The image was made with data collected by the Tropical Rainfall Measuring Mission (TRMM) satellite between August 20 and September 21, 2007. The average daily totals recorded during this period are compared with average rainfall totals recorded during the same period since TRMM’s launch in 1997.

Regions that received more rain per day than average are blue and green, while places that received less rain would be red, orange, or yellow. The image reveals that most of the Sahel received more rain per day than average in August and September. Some places, marked with pale blue, got as much as 15 millimeters more rain than average per day. The northern Sahel, by contrast, was slightly drier than average, as indicated by its pale yellow tint.

The unusually heavy rains caused flooding in as many as 17 countries and affected more than a million people across Africa. … For those areas that escaped flooding, the rains were beneficial, since farmers in the Sahel rely on rain to water their crops, reported the Famine Early Warning System Network on September 19.

For more on the flooding see BBC news Sept 19th, and BBC news Sept 21st.

A damaged world vs. a severely damaged world

The full report from the IPCC Impacts, adaptation and vulnerability working group is now available (it can be downloaded from their website). Martin Parry, co-chairman of the working group says:

“The choice is now between a future with a damaged world and a future with a severely damaged world,” said Professor Martin Parry, of the Met Office and joint chairman of [IPCC working group 2 – Impacts, adaptation and vulnerability]. “It’s quite striking how big the challenge is. It’s not so long ago that we were all talking about how our children and grandchildren would be affected by climate change. Now, looking at this evidence, it’s in our own lifetimes.” (via 3quarksdaily)

In the report Chapter 20: Perspectives on Climate Change and Sustainability contains Table 20.8 and 20.9 that summarize some of the expected amount of climate change expected for different emissions scenarios and the consquences of those those changes. Click on the images below to see the fullsize versions.

highway to hell

Table 20.8 – global impacts

highway to hell - regional version

Table 20.9 – regional impacts

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.

Catastrophe Bonds: Markets, Learning and Volatility

“Wall Street is a machine for turning information nobody cares about into information people can get rich from.” Michael Lewis, author of Liar’s Poker, Aug 26 NYTimes in his article about catatrophe bonds – which are used to share disaster lossses – Nature’s Casino:

From Miami to San Francisco, the nation’s priciest real estate now faced beaches and straddled fault lines; its most vibrant cities occupied its most hazardous land. If, after World War II, you had set out to redistribute wealth to maximize the sums that might be lost to nature, you couldn’t have done much better than Americans had done. And virtually no one — not even the weather bookies — fully understood the true odds.

But there was an exception: an American so improbably prepared for the havoc Tropical Depression 12 was about to wreak that he might as well have planned it. His name was John Seo, he was 39 years old and he ran a hedge fund in Westport, Conn., whose chief purpose was to persuade investors to think about catastrophe in the same peculiar way that he did. He had invested nearly a billion dollars of other people’s money in buying what are known as “cat bonds.” The buyer of a catastrophe bond is effectively selling catastrophe insurance. He puts down his money and will lose it all if some specified bad thing happens within a predetermined number of years: a big hurricane hitting Miami, say, or some insurance company losing more than $1 billion on any single natural disaster. In exchange, the cat-bond seller — an insurance company looking to insure itself against extreme losses — pays the buyer a high rate of interest.

everywhere he goes, he has been drawn to a similar thorny problem: the right price to charge to insure against potential losses from extremely unlikely financial events. “Tail risk,” as it is known to quantitative traders, for where it falls in a bell-shaped probability curve. Tail risk, broadly speaking, is whatever financial cataclysm is believed by markets to have a 1 percent chance or less of happening. In the foreign-exchange market, the tail event might be the dollar falling by one-third in a year; in the bond market, it might be interest rates moving 3 percent in six months; in the stock market, it might be a 30 percent crash. “If there’s been a theme to John’s life,” says his brother Nelson, “it’s pricing tail.”

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Hirschman’s Rhetoric of Reaction

HirschmanOn the Ecological Economics weblog Dave Iverson reminds us of the great American economist Albert Hirschman‘s book The Rhetoric of Reaction: Perversity, Futility, Jeopardy.

Iverson writes on Hirschman’s thoughts on dialogue and democracy:

As I read it, I wondered, once again, “How many economic arguments are simply the stuff of reactionary rhetoric?” Too many, I fear.

In The Rhetoric of Reaction, Hirschman gives us three theses to ponder:

  • The Perversity Thesis: reform efforts will backfire, tending toward effects opposite those desired
  • The Futility Thesis: reform efforts are doomed to fail from the get-go
  • The Jeopardy Thesis: reform efforts will unravel earlier (better) reforms, or they will unravel the entirety of whatever system is in play…

Hirschman explains how easily both conservatives and progressives get drawn into the rhetorical standoffs, impasses really: “… To the dangers of action it is always possible to oppose the dangers of inaction. …” Here is how Hirschman frames a hypothetical point/counterpoint:

Reactionary: The contemplated action will bring disastrous consequences.

Progressive: Not to take the contemplated action will ring disastrous consequences.

Reactionary: The new reform will jeopardize the older one.

Progressive: The new and the old reforms will mutually reinforce each others.

Reactionary: The contemplated action attempts to change permanent structural characteristics ([natural] “laws”) of the social order; it is therefore bound to be wholly ineffective, futile.

Progressive; The contemplated action is backed up by powerful historical forces that are already “on the march”; opposing them would be utterly futile.

Hirschman concludes with:

Recent reflection on democracy have yielded two valuable insights …. Modern pluralistic regimes have typically come into being not because of some preexisting wide consensus on “basic values,” bur rather because various groups that had been at each others’ throats for a prolonged period had to recognize their mutual inability to achieve dominance. Tolerance and acceptance of pluralism resulted eventually from a standoff between bitterly hostile opposing groups.

This historical point of departure of democracy does not bode particularly well for the stability of these regimes. The point is immediately obvious, but it becomes even more so when it is brought into contact with the theoretical claim that a democratic regime achieves legitimacy to the extent that its decisions result from full and open deliberation among its principal groups, bodies, and representatives. Deliberation is here conceived, as an opinion-forming process: the participants should not have fully or definitively formed opinions at the outset; they are expected to engage in meaningful discussion, which means that they should be ready to modify initially held opinions in the light of arguments of other participants and also as a result of new information which becomes available in the course of the debate. …

If this is what it takes for the democratic process to become self-sustaining and to acquire long-run stability and legitimacy, then the gulf that separates such a state from democratic-pluralistic regimes as they emerge historically from strife and civil war is uncomfortably and perilously wide. A people that only yesterday was engaged in fratricidal struggles is not likely to settle down overnight to those constructive give-and-take deliberations. Far more likely , there will initially be agreement to disagree, but without any attempt at melding the opposing points of view—that is indeed the nature of religious tolerance. Or, if there is discussion, it will be a typical “dialogue of the deaf”—a dialogue that will in fact long function as a prolongation of, and a substitute for, civil war. Even in the most “advanced” democracies, many debates are, to paraphrase Clausewitz, a “continuation of civil war with other means.” Such debates, with each part on the lookout for arguments that kill, are only too familiar from democratic politics as usual.

There remains then a long and difficult road to be traveled from the traditional internecine, intransigent discourse to a more “democracy-friendly” kind of dialogue. …

One question lingers with me: How far have we, particularly here in the US, backpedaled in our quest for pluralistic reasoning?

When “values” of various stripes are trotted out before us on a daily basis, asking us to pledge allegiance to ‘values’ framed as ‘moral absolutes’ in-ever-more-strident urgings, why are we not in the streets screaming, Stop! We are losing the very platform on which democracy can flourish!

Or maybe I’m just being reactionary?