I, Robot

24 January, 2012

On 13 February 2012, I will give a talk at Google in the form of a robot. I will look like this:


My talk will be about “Energy, the Environment and What We Can Do.” Since I think we should cut unnecessary travel, I decided to stay here in Singapore and use a telepresence robot instead of flying to California.

I thank Mike Stay for arranging this at Google, and I especially thank Trevor Blackwell and everyone else at Anybots for letting me use one of their robots!

I believe Google will film this event and make a video available. But I hope reporters attend, because it should be fun, and I plan to describe some ways we can slash carbon emissions.

More detail: I will give this talk at 4 pm Monday, February 13, 2012 in the Paramaribo Room on the Google campus (Building 42, Floor 2). Visitors and reporters are invited, but they need to check in at the main visitor’s lounge in Building 43, and they’ll need to be escorted to and from the talk, so someone will pick them up 10 or 15 minutes before the talk starts.

Energy, the Environment and What We Can Do

Abstract: Our heavy reliance on fossil fuels is causing two serious problems: global warming, and the decline of cheaply available oil reserves. Unfortunately the second problem will not cancel out the first. Each one individually seems extremely hard to solve, and taken
together they demand a major worldwide effort starting now. After an overview of these problems, we turn to the question: what can we do about them?

I also need help from all of you reading this! I want to talk about solutions, not just problems—and given my audience, and the political deadlock in the US, I especially want to talk about innovative solutions that come from individuals and companies, not governments.

Can changing whole systems produce massive cuts in carbon emissions, in a way that spreads virally rather than being imposed through top-down directives? It’s possible. Curtis Faith has some inspiring thoughts on this:

I’ve been looking on various transportation and energy and environment issues for more than 5 years, and almost no one gets the idea that we can radically reduce consumption if we look at the complete systems. In economic terms, we currently have a suboptimal Nash Equilibrium with a diminishing pie when an optimal expanding pie equilibrium is possible. Just tossing around ideas a a very high level with back of the envelope estimates we can get orders of magnitude improvements with systemic changes that will make people’s lives better if we can loosen up the grip of the big corporations and government.

To borrow a physics analogy, the Nash Equilibrium is a bit like a multi-dimensional metastable state where the system is locked into a high energy configuration and any local attempts to make the change revert to the higher energy configuration locally, so it would require sufficient energy or energy in exactly the right form to move all the different metastable states off their equilibrium either simultaneously or in a cascade.

Ideally, we find the right set of systemic economic changes that can have a cascade effect, so that they are locally systemically optimal and can compete more effectively within the larger system where the Nash Equilibrium dominates. I hope I haven’t mixed up too many terms from too many fields and confused things. These terms all have overlapping and sometimes very different meaning in the different contexts as I’m sure is true even within math and science.

One great example is transportation. We assume we need electric cars or biofuel or some such thing. But the very assumption that a car is necessary is flawed. Why do people want cars? Give them a better alternative and they’ll stop wanting cars. Now, what that might be? Public transportation? No. All the money spent building a 2,000 kg vehicle to accelerate and decelerate a few hundred kg and then to replace that vehicle on a regular basis can be saved if we eliminate the need for cars.

The best alternative to cars is walking, or walking on inclined pathways up and down so we get exercise. Why don’t people walk? Not because they don’t want to but because our cities and towns have optimized for cars. Create walkable neighborhoods and give people jobs near their home and you eliminate the need for cars. I live in Savannah, GA in a very tiny place. I never use the car. Perhaps 5 miles a week. And even that wouldn’t be necessary with the right supplemental business structures to provide services more efficiently.

Or electricity for A/C. Everyone lives isolated in structures that are very inefficient to heat. Large community structures could be air conditioned naturally using various techniques and that could cut electricity demand by 50% for neighborhoods. Shade trees are better than insulation.

Or how about moving virtually entire cities to cooler climates during the hot months? That is what people used to do. Take a train North for the summer. If the destinations are low-resource destinations, this can be a huge reduction for the city. Again, getting to this state is hard without changing a lot of parts together.

These problems are not technical, or political, they are economic. We need the economic systems that support these alternatives. People want them. We’ll all be happier and use far less resources (and money). The economic system needs to be changed, and that isn’t going to happen with politics, it will happen with economic innovation. We tend to think of our current models as the way things are, but they aren’t. Most of the status quo is comprised of human inventions, money, fractional reserve banking, corporations, etc. They all brought specific improvements that made them more effective at the time they were introduce because of the conditions during those times. Our times too are different. Some new models will work much better for solving our current problems.

Your idea really starts to address the reason why people fly unnecessarily. This change in perspective is important. What if we went back to sailing ships? And instead of flying we took long leisurely educational seminar cruises on modern versions of sail yachts? What if we improved our trains? But we need to start from scratch and design new systems so they work together effectively. Why are we stuck with models of cities based on the 19th-century norms?

We aren’t, but too many people think we are because the scope of their job or academic career is just the piece of a system, not the system itself.

System level design thinking is the key to making the difference we need. Changes to the complete systems can have order of magnitude improvements. Changes to the parts will have us fighting for tens of percentages.

Do you know good references on ideas like this—preferably with actual numbers? I’ve done some research, but I feel I must be missing a lot of things.

This book, for example, is interesting:

• Michael Peters, Shane Fudge and Tim Jackson, editors, Low Carbon Communities: Imaginative Approaches to Combating Climate Change Locally, Edward Elgar Publishing Group, Cheltenham, UK, 2010.

but I wish it had more numbers on how much carbon emissions were cut by some of the projects they describe: Energy Conscious Households in Action, the HadLOW CARBON Community, the Transition Network, and so on.


Melting Permafrost (Part 3)

19 December, 2011

Melting permafrost is in the news! Check out this great slide show and article:

• Josh Hane, Hunting for clues to global warming, New York Times, 16 December 2011.

• Justin Gillis, As permafrost thaws, scientists study the risks, New York Times, 16 December 2011.

They track Katey M. Walter Anthony, an assistant professor at the Water and Environmental Research Center at the University of Alaska Fairbanks, as she studies methane bubbling up from lakes—as shown above.

These lakes form in an interesting way. Permafrost is permanently frozen soil lying beneath a layer 0.6 to 4 meters thick of soil that thaws in the summer and refreezes in the winter: the active layer. The permafrost itself can be much thicker—up to 1500 meters in parts of Siberia!

As far as I can tell, talik is permanently unfrozen soil on top of, amid or beneath the permafrost.

Permafrost is rock-hard and solid. Liquid water does not pass through it, so permafrost environments tend to be poorly drained and boggy. But when permafrost starts to melt, it becomes soft. Soil sinks down into marshy hollows separated by small hills, forming a kind of terrain called thermokarst.

Trees in this terrain can lean crazily as their roots sink, creating drunken forests.

On flat ground, melted water can pool into a thermokarst lake. On slopes, water pours downhill and the land can rip open in a thermokarst failure. Here are Breck Bowden and Michael Gooseff exploring a thermokarst failure in Alaska:

For more on this, see:

• Emily Stone, When the ground collapses like a soufflé: Studying the effect of thermokarst on the Arctic, Field Notes: the Polar Field Services Newsletter

All these are natural processes that are widespread at the end of each glacial period. Here’s a surprisingly delightful book which discusses this in detail:

• Evelyn C. Pielou, After the Ice Age: the Return of Life to Glaciated North America, U. Chicago Press, Chicago, 1991.

So, please don’t misunderstand: I’m not trying to say that thermokarst lakes, drunken forests and the like are signs of disaster. However, as the Earth warms, new regions of permafrost are melting, and we’ll see these phenomena in new regions. We need to understand how they work, and the positive and negative feedbacks. For example, thermokarst lakes are darker than their surroundings, so they absorb more sunlight and warm the area.

Most importantly, as permafrost thaws, it releases trapped carbon in the form of carbon dioxide and methane, which are both greenhouse gases. Since there are roughly 1.7 trillion tons of carbon in northern soils, with about 90% locked in permafrost, that’s a big deal.

At least once so far, the tundra has even caught fire:

One day in 2007, on the plain in northern Alaska, a lightning strike set the tundra on fire.

Historically, tundra, a landscape of lichens, mosses and delicate plants, was too damp to burn. But the climate in the area is warming and drying, and fires in both the tundra and forest regions of Alaska are increasing.

The Anaktuvuk River fire burned about 400 square miles of tundra, and work on lake sediments showed that no fire of that scale had occurred in the region in at least 5,000 years.

Scientists have calculated that the fire and its aftermath sent a huge pulse of carbon into the air — as much as would be emitted in two years by a city the size of Miami. Scientists say the fire thawed the upper layer of permafrost and set off what they fear will be permanent shifts in the landscape.

Up to now, the Arctic has been absorbing carbon, on balance, and was once expected to keep doing so throughout this century. But recent analyses suggest that the permafrost thaw could turn the Arctic into a net source of carbon, possibly within a decade or two, and those studies did not account for fire.

“I maintain that the fastest way you’re going to lose permafrost and release permafrost carbon to the atmosphere is increasing fire frequency,” said Michelle C. Mack, a University of Florida scientist who is studying the Anaktuvuk fire. “It’s a rapid and catastrophic way you could completely change everything.”

By the way, if you click on these scientists’ portraits, you’ll see where they work. If you’re a student looking for an interesting career, consider these options! For example, Michelle C. Mack—shown above—runs a lab, and you can see her postdocs and grad students, and what they do.

For previous posts in this series, see:

Melting Permafrost (Part 1).

Melting Permafrost (Part 2).


Melting Permafrost (Part 2)

14 December, 2011

This summer a Russian research ship found hundreds of plumes of methane, “of a fantastic scale”, bubbling up from the sea floor off the East Siberian coast:

• Steve Connor, Shock as retreat of Arctic sea ice releases deadly greenhouse gas, 13 December 2011.

Here are the quotes with actual new information:

In late summer, the Russian research vessel Academician Lavrentiev conducted an extensive survey of about 10,000 square miles of sea off the East Siberian coast. Scientists deployed four highly sensitive instruments, both seismic and acoustic, to monitor the “fountains” or plumes of methane bubbles rising to the sea surface from beneath the seabed.

“In a very small area, less than 10,000 square miles, we have counted more than 100 fountains, or torch-like structures, bubbling through the water column and injected directly into the atmosphere from the seabed,” Dr Semiletov said. “We carried out checks at about 115 stationary points and discovered methane fields of a fantastic scale – I think on a scale not seen before. Some plumes were a kilometre or more wide and the emissions went directly into the atmosphere – the concentration was a hundred times higher than normal.”

and

“This is the first time that we’ve found continuous, powerful and impressive seeping structures, more than 1,000 metres in diameter. It’s amazing,” Dr Semiletov said. “I was most impressed by the sheer scale and high density of the plumes. Over a relatively small area we found more than 100, but over a wider area there should be thousands of them.”

Scientists estimate that there are hundreds of millions of tonnes of methane gas locked away beneath the Arctic permafrost, which extends from the mainland into the seabed of the relatively shallow sea of the East Siberian Arctic Shelf. One of the greatest fears is that with the disappearance of the Arctic sea-ice in summer, and rapidly rising temperatures across the entire region, which are already melting the Siberian permafrost, the trapped methane could be suddenly released into the atmosphere leading to rapid and severe climate change.

Dr Semiletov’s team published a study in 2010 estimating that the methane emissions from this region were about eight million tonnes a year, but the latest expedition suggests this is a significant underestimate of the phenomenon.

I’d like to know more about Igor Semiletov’s work and what he’s just found. He was mentioned in this earlier very good article:

• Amanda Leigh Mascarelli, A sleeping giant?, Nature Reports Climate Change, 5 March 2009.

Namely:

The Siberian Shelf alone harbours an estimated 1,400 billion tonnes of methane in gas hydrates, about twice as much carbon as is contained in all the trees, grasses and flowers on the planet. If just one per cent of this escaped into the atmosphere within a few decades, it would be enough to cause abrupt climate change, says Shakhova. “When hydrates are destabilized, gas is released under very high pressure,” she says. “So emissions could be massive and non-gradual.” Shakhova and her colleague Igor Semiletov of the University of Alaska, Fairbanks, believe the plumes they’ve observed confirm previous reports that the permafrost cap is beginning to destabilize, allowing methane to escape from the frozen hydrates below. “Subsea permafrost is like a rock,” explains Semiletov. “It works like a lid to prevent escape of any gas. We believe that the subsea permafrost is failing to seal the ancient carbon pool.”

But Carolyn Ruppel, a geophysicist with the US Geological Survey in Woods Hole, Massachusetts, isn’t yet ready to attribute the methane plumes to a breakdown in methane hydrates in the subsea permafrost. “We have proof from studies that have been carried out in the past few years that there’s a lot of methane in certain shallow marine environments offshore in the Arctic,” says Ruppel. “But can we prove that the methane comes from methane hydrates? That is a critical question.”

Why is it critical? Because people are worried about global warming melting permafrost and gas hydrates on the ocean floor. Suppose these release large amounts of methane, a greenhouse gas vastly more potent than carbon dioxide. This will then makes the Earth even warmer, and so on: we have a feedback loop. In a real nightmare scenario, we could imagine that this feedback actually leads to a ‘tipping point’, where the climate flips over to a much warmer state. And in the worst nightmare of all, we can imagine something like Paleocene-Eocene Thermal Maximum, a spike of heat that lasted about 20,000 years, causing significant extinctions.

Are any of these nightmares really possible? I wrote about this question before, assembling what facts I could easily find:

Melting permafrost (Part 1).

How much new light does Semiletov’s work shed on this question?

Luckily, a team of scientists is gearing up to answer it:

Permafrost Carbon Network (RCN).

Here’s a paper by this team:

• Edward A. G. Schuur, Benjamin Abbott and the Permafrost Carbon Network, High risk of permafrost thaw, Nature 480 (1 December 2011), 32-33.

To get the ball rolling, they surveyed themselves. That may seem like a lazy way to write a paper, but I don’t mind it as a quick way to get a sense of the conventional wisdom… and they probably wanted to do it just to find out what they all thought! Here are the results—emphasis mine:

Our survey asks what percentage of the surface permafrost is likely to thaw, how much carbon will be released, and how much of that carbon will be CH4, for three time periods and under four warming scenarios that will be part of the Intergovernmental Panel on Climate Change Fifth Assessment Report. The lowest warming scenario projects 1.5 °C Arctic warming over the 1985–2004 average by the year 2040, ramping up to 2 °C by 2100; the highest warming scenario considers 2.5 °C by 2040, and 7.5 °C by 2100. In all cases, we posited that the temperature would remain steady from 2100 to 2300 so that we could assess opinions about the time lag in the response of permafrost carbon to temperature change.

The survey was filled out this year by 41 international scientists, listed as authors here, who publish on various aspects of permafrost. The results are striking. Collectively, we hypothesize that the high warming scenario will degrade 9–15% of the top 3 metres of permafrost by 2040, increasing to 47–61% by 2100 and 67–79% by 2300 (these ranges are the 95% confidence intervals around the group’s mean estimate). The estimated carbon release from this degradation is 30 billion to 63 billion tonnes of carbon by 2040, reaching 232 billion to 380 billion tonnes by 2100 and 549 billion to 865 billion tonnes by 2300. These values, expressed in CO2 equivalents, combine the effect of carbon released as both CO2 and as CH4.

Our estimate for the amount of carbon released by 2100 is 1.7–5.2 times larger than those reported in several recent modelling studies, all of which used a similar warming scenario. This reflects, in part, our perceived importance of the abrupt thaw processes, as well as our heightened awareness of deep carbon pools. Active research is aimed at incorporating these main issues, along with others, into models.

Are our projected rapid changes to the permafrost soil carbon pool plausible? The survey predicts a 7–11% drop in the size of the permafrost carbon pool by 2100 under the high-warming scenario. That scale of carbon loss has happened before: a 7–14% decrease has been measured in soil carbon inventories across thousands of sites in the temperate-zone United Kingdom as a result of climate change. Also, data scaled up from a single permafrost field site point to a potential 5% loss over a century as a result of widespread permafrost thaw. These field results generally agree with the collective carbon-loss projection made by this survey, so it should indeed be plausible.

Across all the warming scenarios, we project that most of the released carbon will be in the form of CO2 with only about 2.7% in the form of CH4. However, because CH4 has a higher global-warming potential, almost half the effect of future permafrost-zone carbon emissions on climate forcing is likely to be from CH4. That is roughly consistent with the tens of billions of tonnes of CH4 thought to have come from oxygen-limited environments in northern ecosystems after the end of the last glacial period.

All this points towards significant carbon releases from permafrost-zone soils over policy-relevant timescales. It also highlights important lags whereby permafrost degradation and carbon emissions are expected to continue for decades or centuries after global temperatures stabilize at new, higher levels. Of course, temperatures might not reach such high levels. Our group’s estimate for carbon release under the lowest warming scenario, although still quite sizeable, is about one-third of that predicted under the strongest warming scenario.

I found this sentence is a bit confusing:

These values, expressed in CO2 equivalents, combine the effect of carbon released as both CO2 and as CH4.

But I guess that combined with a guess like “30 billion to 63 billion tonnes of carbon by 2040”, it means that they’re expecting a release of carbon dioxide and methane that’s equal, in its global warming potential, to what you’d get from burning 30 to 63 billion tonnes of carbon, turning it all into carbon dioxide, and releasing it into the atmosphere.

For comparison, in 2010 humanity burnt 8.3 billion tonnes of carbon. So, at least up to 2040, I guess they’re expecting the effect of melting permafrost to be roughly 1/8 to 1/4 of the direct effect of burning carbon.


A Bet Concerning Neutrinos

27 September, 2011

Over on Google+ I wrote:

I’m willing to take bets that this faster-than-light neutrino business will turn out to be wrong. We can negotiate the detailed terms, the odds, and the stakes.

But beware: I’m still enjoying the case of scotch I won from David Ring. I bet there’d be no “strong evidence for supersymmetry” within the first year of operation of the Large Hadron Collider.

It took a couple of days, but I finally got someone willing to take me up on this. And—surprise!—it was none other than Frederick De Roo, one of the key contributors to the Azimuth Project.

But he’s playing for higher stakes than I’d expected:

Hi John,

actually I’m willing to take a bet.

I propose to bet (even though I don’t believe it) that

neutrinos can go faster than light

The loser of the bet will promise to the winner not to fly for one whole year! (for a year chosen within a specified number of years after the bet has expired)

How about that? The earth wins regardless who’s right ;-)

I asked him if we could discuss the details here, and he said okay.

It’s a tricky business. While I’ve got the odds on my side, I’ve also got more to lose!

Frederik lives in Europe, where there are lots of trains. His idea of a fun vacation is a month-long bike trip. What’s he got to lose?

I could easily survive a year of not flying to conferences. It would hurt a bit. Still, I’d say yes in a minute if it were just up to me. But Lisa and I have permanent positions at the University of California in Riverside, and we’re trying to work out a deal where we work in Singapore every summer. So, I can’t really agree to this bet unless I get her okay!

How do I convince a non-physicist—and not just any non-physicist, but my wife—that it’s really, really safe to bet a summer of being together on the possibility that neutrinos go faster than light?

We spent seven years on opposite sides of the country before she got a job at UC Riverside. We promised we’d never do something like that again. And now I’m saying “oh, don’t worry, dear: special relativity is very well tested.” If you haven’t been in this situation, you don’t know how unconvincing that sounds.

Should I look into cruises from Southern California to Singapore? How long do those take, anyway? It would be a bummer to get there only have to head straight back.

What would you say, Frederik, if I changed the the terms of the bet to something like this? If I lose the bet, for each plane trip I take during the specified year, I’ll donate $10,000 to your favorite environmental organization. Carbon offsets, or whatever you like. That way if I lose, I suffer, but not my marriage.


American Oil Boom?

26 September, 2011

If this is for real, it’s the biggest news I’ve heard for a long time:

Two years ago, America was importing about two thirds of its oil. Today, according to the Energy Information Administration, it imports less than half. And by 2017, investment bank Goldman Sachs predicts the US could be poised to pass Saudi Arabia and overtake Russia as the world’s largest oil producer.

This is from:

New boom reshapes oil world, rocks North Dakota, All Things Considered, National Public Radio, 25 September, 2011.

The new boom is due to technologies like fracking (short for hydraulic fracturing) and directional drilling. According to an estimate in this article, in the last few years advances in these technologies have made available up to 11 billion barrels of oil in the Bakken formation under North Dakota and Montana. There’s also a lot under the Canadian side of the border:

This map is from:

• Jerry Langton, Bakken Formation: Will it fuel Canada’s oil industry?, CBC News, 27 June 2008.

How big is this boom going to be? What will it mean? The National Public Radio story says this:

Amy Myers Jaffe of Rice University says in the next decade, new oil in the US, Canada and South America could change the center of gravity of the entire global energy supply.

“Some are now saying, in five or 10 years’ time, we’re a major oil-producing region, where our production is going up,” she says.

The US, Jaffe says, could have 2 trillion barrels of oil waiting to be drilled. South America could hold another 2 trillion. And Canada? 2.4 trillion. That’s compared to just 1.2 trillion in the Middle East and north Africa.

Jaffe says those new oil reserves, combined with growing turmoil in the Middle East, will “absolutely propel more and more investment into the energy resources in the Americas.”

Russia is already feeling the growth of American energy, Jaffe says. As the U.S. produces more of its own natural gas, Europe is free to purchase liquefied natural gas the US is no longer buying.

“They’re buying less natural gas from Russia,” Jaffe says. “So Russia would only supply 10 percent of European natural gas demand by 2030. That means the Russians are no longer powerful.”

The American energy boom, Jaffe says, could endanger many green-energy initiatives that have gained popularity in recent years. But royalties and revenue from U.S. production of oil and natural gas, she adds, could be used to invest in improving green technology.

What do you know about this news? Is it for real, is it being hyped? What do the smartest of the ‘peak oil’ crowd say?

I’ve read about the environmental impacts of fracking, and the consequences for global warming are evident. Since ‘carbon is forever’, to reduce carbon dioxide levels we need to either stop burning carbon or figure out a way to sequester CO2. A new oil boom won’t help us with that. And in the long run, we’ll still run out.

But the short run could last decades. Suppose people go ahead, ignore the dangers, and ‘drill, baby, drill’. How will geopolitics, the world economy, and the environment be affected?

Opinions are fine—everyone’s got one—but facts are better… and facts with references are the best.


Climate Reality Project

14 September, 2011

The Climate Reality Project is planning a presentation called “24 Hours of Reality” beginning at 7 pm Central Time on September 14th, arguing for the connection between more extreme weather and climate change. “There will be a full-on assault on climate skeptics, exploring where they get their funding from.”

The Washington Post has an interview with Al Gore about this project:

• Brad Plumer, Al Gore: ‘The message still has to be about the reality we’re facing’ , Washington Post, 12 September 2011.

I’ll quote a bit:

Brad Plumer: “An Inconvenient Truth” was basically a primer on global warming—the causes, the problems it creates, the ways we can avert it. So what more is there to add? How will this new presentation be different?

Al Gore: It’s very different—a few of the images are the same, but 95 percent of the slides are completely new. The science linking the increased frequency and severity of extreme weather to the climate crisis has matured tremendously in the last couple of years. Think about the last year, we’ve had floods in Pakistan displacing 20 million people and further destabilizing a nuclear-armed country. We’ve had drought and wildfires in Russia. In Australia you’ve got floods the size of France and Germany combined. Then there’s drought in Texas—out of 254 counties in Texas, 252 are on fire. I’m talking to you from Nashville, where the city lost the equivalent of an entire year’s budget from recent floods—the area has never been flooded like this before, so no one had flood insurance.

That’s the reality we’ve got to focus on. This presentation is a defense of the science and the scientists, against the timeworn claims by deniers.

BP: Now, whenever a natural disaster happens—say, a flood or a wildfire—you typically see scientists quoted in the press saying, “Well, it’s hard to attribute any single event to global warming, although this is the sort of event we should see more of as the planet warms.” As I understand it, this sort of extra-careful hedge is becoming outdated. Scientists actually are making tighter connections between current disasters and climate change, correct?

AG: Yes, that shift in the way scientists describe the linkage is one of the elements of this new slideshow. It’s a subtle but extremely important shift. They used to say that the climate crisis changes the odds of extreme weather events—this was the old metaphor of “loading the dice.” Now, they say there’s not only a greater likelihood of rolling 12s, but we’re actually loading 13s and could soon be rolling 15s and 16s. As scientists like James Hansen [of NASA’s Goddard Institute for Space Studies] and Kevin Trenberth [of the National Center for Atmospheric Research] point out, the changes brought about by man-made global-warming pollution have reached the stage that every event is now being affected by it in some way.

In the last 30 years, for instance, we’ve seen water vapor above the oceans increase by 4 percent, and many storms reach as far as 2,000 miles out to collect water vapor. So when you have a 4 percent increase over such a large area, the storms are now fueled with more water vapor than was the case 30 years ago. That means we’re getting larger downpours. And in drought-prone areas, we’re seeing increasing intervals between downpours, which is one of several reasons why we’re seeing extreme droughts.

BP: Now, you’re talking about presenting the stark facts as a way of persuading people that climate change is a problem. Yet when you look at polls on climate belief, one thing that stands out is that the people most dismissive of global warming tend to be the most confident that they have all the information they need. Doesn’t that suggest there’s a point at which more information doesn’t actually persuade anyone?

AG: Well, that logic hasn’t led deniers to stop pressing the inaccurate disinformation about climate science. And the fact is that quite a few of the large carbon polluters and their allies in the ideological right wing have been spending hundreds of millions of dollars per year to mislead people. Have you read Naomi Oreske’s book Merchants of Doubt? The tobacco companies a few decades ago pioneered this organized disinformation technique to create artificial doubt about the science of their product—they hired actors to dress them up as doctors and had them say, “I’m a doctor, there’s nothing wrong with smoking cigarettes; in fact, it’ll make you feel better.” And some of the same people who took money from tobacco companies to lie about tobacco science are now taking money from large carbon polluters to lie about the reality of the climate crisis.

BP: Okay, but taking that opposition is a given, there’s been a lot of discussion about whether something more is needed to fight it than yet another recital of climate science facts.

AG: Right, you hear a lot of people giving advice on how to talk about climate science—how you need to dress differently or stand on your head and deliver the message in rhyme. And I respect all that, and I hope a lot of people will present the message in their own way. But my message is about presenting the reality. I have faith in the United States and our ability to make good decisions based on the facts. And I believe Mother Nature is speaking very loudly and clearly. We’ve had ten disasters in the United States this year alone costing more than $1 billion and which were climate-related. It’s only a matter of time before reality sinks in, and we need both parties involved. And the only way to get the right answer is to understand the question.


Australian Carbon Tax

13 July, 2011

Australians burn a lot of carbon. Per person, they’re right up there with Americans:

The map here is based on data from 2000. In 2008, Australians spewed out 18.9 tonnes of CO2 per person in the process of burning fossil fuels and making cement. Americans spewed 17.5 tonnes per person. The world average was just 4.4.

Australians also mine a lot of coal. It’s their biggest export! On top of that, coal exports have more than doubled in recent years:

Last Sunday, however, Prime Minister Julia Gillard announced a tax on carbon!

In this scheme, the 500 biggest polluters in Australia will be taxed at AU $23 per tonne of carbon emissions starting in July 2012. The price will increase 2.5% each year until 2015, and then a carbon trading scheme will be introduced. The hope is that by 2020, Australian carbon emissions will drop 5% below 2000 levels.

Of course, the further we go into the future, the less sure we can be of anything. What if Gillard’s party gets voted out of power? There’s already considerable dissatisfaction with Gillard’s plan, in part because she had earlier said:

There will be no carbon tax under the Government I lead.

but mainly, of course, because taxes are unpopular and the coal lobby is very strong in Australia. There’s been a lot of talk about how the carbon tax will hurt the economy.

These objections are to be expected, and thus not terribly interesting (even if they’re valid). However, some more interesting objections are posed here:

• Annabel Crab, Australia’s diabolical carbon pricing scheme, ABC News, 13 July 2010.

First, it seems that Prime Minister Gillard favors continuing to sell lots of coal to other countries. As she recently said:

Tony Abbott was predicting Armageddon for the coal mining industry But the future of coal mining in Australia is bright.

But coal mining can’t really have a ‘bright future’ in a decarbonized world unless we capture and store the carbon dioxide emitted by coal-burning plants.

Second, in the planned carbon trading scheme beginning in 2015, Australian companies will be allowed to account for half of their emissions reductions by simply buying permits from overseas. I’m not sure this is bad: it could simply be efficient. However, Annabel Crab points out that it has some seemingly paradoxical effects. She quotes a Treasury document saying:

In a world where other countries pursue more ambitious abatement targets, the carbon price will be higher, and this increases the cost in terms of domestic production and income foregone.

Is this really bad? I’m not sure. I hope however that the Australian carbon tax goes forward to the point where we can see its effects instead of merely speculate about them.


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