Gorbachev on climate change and the Berlin Wall

Mikhail Gorbachev has written an article for The Times arguing that there are similarities between the battle against climate change today and the fall of the Berlin Wall twenty years ago:

Addressing climate change demands a paradigm shift on a scale akin to that required to end the Cold War. But we need a “circuit-breaker” to escape from the business-as-usual that currently dominates the political agenda. It was the transformation brought about by perestroika and glasnost that provided the quantum leap for freedom for the Soviet Union and Eastern Europe, and opened the way for the democratic revolution that saved history. Climate change is complex and closely entwined with a host of other challenges, but a similar breakthrough in our values and priorities is needed.

There is not just one wall to topple, but many. There is the wall between those states which are already industrialised, and those developing countries which do not want to be held back. There is the wall between those who cause climate change, and those who suffer the consequences. There is the wall between those who heed the scientific evidence, and those who pander to vested interests. And there is the wall between the citizens who are changing their own behaviour and want strong global action, and the leaders who are so far letting them down.

He also calls on the leaders of the US, UK, India and China to attend the Copenhagen summit personally.

Of course, there are major differences between the two cases. The Berlin Wall was effectively a mechanism to hold people back from acting as they wished to, halting the movement of people from East to West Germany, and beyond. Dealing with climate change isn’t about allowing the energy people already have to be put into application, but rather about encouraging and compelling them to behave in better ways, largely for the welfare of others. That being said, it is good to see the historic importance of success or failure on this issue recognized. Hopefully, Copenhagen will go better than people are predicting.

Why conservatives should love carbon taxes

Climate emergency

The National Post – Canada’s right-leaning daily newspaper – has publicly stated that it believes climate change is real, and also that the current government has the right approach to dealing with it. In particular, it praises Environment Minister Jim Prentice for avoiding the “creation of state-managed “green economies” — socialism with a Gaian face.”

Whether such a creation is possible (and whether it would be desirable or not) are questions that can be set aside for a moment. The irony that seems to be paramount when it comes to the relationship between conservatives and climate change is how they stress a desire to interfere in markets and individual choices as little as possible, while rejecting the mechanism that would do that best: a carbon tax. A carbon tax doesn’t force anyone to drive a small car or, terrifying thought, forgo automobiles all together. It doesn’t force people to choose small pets, give up flying, or make other specific sacrifices. It also doesn’t rely upon the government deciding which energy technologies should succeed, whether that means renewables, nuclear, carbon capture and storage, or something else. It encourages low-carbon technological development in the most hands-off and market-friendly way possible.

All a carbon tax does is take the price imposed on strangers by greenhouse gas emissions and makes it ‘internal’ to the decision-making of individuals and other economic actors throughout society. It comes the closest to retaining the libertarian ideal in a world where interconnectedness forces us to take into consideration the consequences our actions will have on others. I have talked before about the irony of how laissez faire climate policies will inevitably fail and force governments to take employ more coercive measures. That outcome can only be avoided by sending a clear price signal on greenhouse gas emissions, and doing so early and at a meaningful level. Indeed, a carbon tax can be said to be a way of protecting property rights, given that it reduces the degree to which emitters will harm the property and prosperity of other people around the world.

It should be noted that the important policy change here is to put a price on carbon emissions, to represent the harm they cause to other people. The establishment of such a price is more important than the precise mechanism through which it is done, whether that is a carbon tax or a cap-and-trade system in which 100% of the permits are sold at auction. The choice of instrument is less important than moving quickly to put a price on carbon in one way or another.

It is an open question whether conservatives will realize the extent to which they are undermining their own aims and ideals through opposition to carbon pricing. Part of that is the paleoconservative stance that climate change isn’t happening, that it is benign, that it is inevitable, etc. Among conservatives with enough basic awareness about the world to know that those arguments have been discredited, we should hope that support begins to grow for the idea of dealing with the climate problem in the way that involves the least expansion of the state and the least infringement on liberty: a carbon tax.

While there may well be cause for accompanying such a tax with other regulations – such as a ban on coal power – at least gaining conservative support for some kind of carbon action would change the tone of the debate. We would finally stop pretending that we can ignore climate change indefinitely while the economy keeps ticking on just fine, and begin to appreciate and implement the steps required to build a low-carbon future.

Arctic sea ice, in the midst of re-freezing

While 2007 retains the record for the lowest observed mimumum summer Arctic sea ice extent, the level right now is the lowest ever observed for this time of year:

Arctic sea ice extent, 9 November 2009

The US National Snow and Ice Data Centre explains the situation with reference to strong winds: “the growth rate slowed for a time in early October, coinciding with strong winds from the south over central Siberia. The winds helped prevent ice from forming along the Siberian coast. At the end of the month, extensive areas of open water regions were still present in the northernmost North Atlantic, and north of Alaska. The ice edge was north of both Svalbard and Franz Josef Land.”

The year-on-year trend, going back more than 30 years, shows that fall ice has been progressively less extensive. Note that, at Canada’s northernmost permanent settlement nautical polar night conditions exist from late November to mid-January. During this time, “no trace of light can be seen anywhere but the sky is not completely dark at midday.” Further north, where the middle of the Arctic icecap is, this period of darkness extends even longer.

From the Cambridge ivory tower to Whitehall

Apparently David MacKay, whose excellent book I reviewed before, has been appointed Chief Scientific Advisor of the Department of Energy and Climate Change in the United Kingdom and given a staff of 50. Apparently, he is advocating that the UK quadruple its nuclear energy capacity, as a stopgap between fossil fuels and the eventual dominance of renewables. Personally, I think it is encouraging that someone who committed so much personal energy to thinking about ways to get off fossil fuels has been given a mandate to help do so, in an official capacity.

My friend Mark let me know about this development.

Climate science and policy-making

I wrote the following to serve as a one-page introduction, laying out some of the key items for consideration and listing some of the most accessible and reputable sources of information about climate change. For more information on specific subjects, see my climate change index.

The key elements of the general climate science and policy consensus are:

  • On average, the planet is warming.
  • Most of this is because of human emissions of greenhouse gases.
  • Continued warming would be harmful, and perhaps very risky when it comes to human welfare and prosperity. Anticipated changes include melting glaciers and polar ice, more extreme precipitation events, agricultural impacts, wildfires, heat waves, increased incidence of some infectious diseases, sea level rise, ocean acidification, and increased hurricane intensity.
  • By most accounts, the cost of mitigation is less than the cost of adaptation. Some anticipated changes may overwhelm the capacity of human and natural systems to adapt.

While there is a public perception that there is a lot of scientific disagreement about the fundamentals of climate science, this really is not the case. Back in 2004, a survey of peer-reviewed work on climate science demonstrated this. There is also a notable joint statement from the national science academies of the G8, Brazil, China, South Africa, and India.

To borrow a phrase from William Whewell, there is a ‘consilience of evidence’ when it comes to the science of climate change: multiple, independent lines of evidence converging on a single coherent account. These forms of evidence are both observational (temperature records, ice core samples, etc) and theoretical (thermodynamics, atmospheric physics, etc). Together, these lines of evidence provide a conceptual and scientific backing to the theory of climate change caused by human greenhouse gas emissions that is simply absent for alternative theories, such as that there is no change or that the change is caused by something different.

Readers who are dubious about the validity of mainstream climate science, or unsure of what to think, my page for waverers may be useful.

1) Climatic science and history

There are some good primers available from reputable organizations online. For instance, the United Kingdom’s Met Office has a quick guide.

The Fourth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC) is the most authoritative review of the scientific work that has been done on climate change. The summary for policy-makers for the synthesis report is available online.

For detailed information on the physical science of climate change, the technical summary of the IPCC’s Working Group I report is a good resource. Unlike the summaries for policy-makers, which are vetted through a quasi-political process, the technical summaries are prepared exclusively by scientists.

For Canadians who want to read one book about climate science and policy, I recommend University of Victoria Professor Andrew Weaver’s book: Keeping Our Cool: Canada in a Warming World.

For those looking for a concise history of the entire development of climatic science, starting in the late 1800s, I very much recommend Spencer Weart’s The Discovery of Global Warming. In addition to the book form, it is available free online.

For a more specific history of what we have learned about climate from ice core samples, see Richard Alley’s The Two Mile Time Machine. For an excellent (though somewhat technical) discussion of the relationships between the carbon cycle and biological organisms, see Oliver Morton’s Eating the Sun.

2) Climate change mitigation

Ultimately, the only way to keep the concentration of greenhouse gases in the atmosphere constant is to reach the point where humanity has zero net emissions. Getting there fundamentally requires two things: the shifting of the energy basis of the global economy to low- and then zero-carbon sources, and the stabilization of the biosphere through actions like ending net deforestation. It is widely accepted that setting a sufficiently high price for greenhouse gas emissions is a vital way to drive mitigation actions.

Three excellent books that evaluate options for moving to a low-carbon economy are:

On the costs of climate change mitigation, the most comprehensive work is probably that which has been done by Nicholas Stern, beginning with the Stern Review. The review’s executive summary is also accessible online. More recently, he has argued that the costs of inaction are even more significant than those projected at that time.

On the political and ethical side of things, the best short summary may be Stephen Gardiner’s article “Ethics and Global Climate Change,” published in Ethics. Volume 114 (2004), p.555-600. One key idea related to international equity and climate change mitigation is contraction and convergence: an arrangement in which the emissions from all states eventually fall to zero, but where the per-capita emissions of developed and developing states also converge over time.

My fantasy climate change policy combines a moratorium on coal and unconventional fossil fuels with a hard cap on emissions.

3) Other major climate change issues

Other areas relevant to climate change policy-making include:

  • Abrupt and runaway climate change scenarios
  • Adaptation to climate change
  • Carbon sinks (physical, such as the oceans, biological, such as the forests, and geological, such as rocks that erode and form carbonates)
  • Economics (carbon pricing, risk management, etc)
  • Emission pathways (and their international breakdown)
  • Equity issues (historical responsibility, climate change and development, etc)
  • Global politics and international law
  • Planning and design (cities, buildings, etc)
  • Science (climatic equilibria, models and projections, etc)
  • Sociological and philosophical issues (ethics, communication, political theory, etc)
  • Targets (stabilization concentrations, temperature change, etc)
  • Technologies (renewable energy, transport, nuclear, efficiency, etc)

I can recommend resources in all of these areas, if someone has a particular interest.

4) Good sources of climate related news

Probably the best scientific climate change blog is RealClimate.

Good responses to climate ‘skeptic’ arguments can be found in the How to Talk to a Climate Skeptic series. I also keep track of my own arguments with climate change deniers.

Climate coverage in mainstream media sources is often inconsistent in quality. The BBC and The Economist often publish good information, but also sometimes include incorrect or misleading information.

5) A few key graphics

Atmospheric concentration of CO2

This ice core record of carbon dioxide concentrations illustrates one major reason why we should be more concerned about human-induced climate change than about natural variation. Our use of fossil fuels is generating a spike in greenhouse gas concentrations that is set to rise far above anything in the last 650,000 years, at least.

Attribution of climate change, from the IPCC 4AR

The above shows how observed warming is inconsistent with climate models that do not incorporate human greenhouse gas emissions, but consistent with those that do.

MIT climate roulette wheels

The wheel on the right depicts researchers’ estimation of the range of probability of potential global temperature change over the next 100 years if no policy change is enacted on curbing greenhouse gas emissions. The wheel on the left assumes that aggressive policy is enacted. (Credit: Image courtesy / MIT Joint Program on the Science and Policy of Global Change)

I would be delighted to answer and questions, or suggest further resources in other areas of interest.

Last updated: 23 January 2012

Oil 101

Twigs and branches

Written essentially in the style of a textbook, Morgan Downey’s Oil 101 moves systematically through the major areas of knowledge required for a basic understanding of the global petroleum industry. These include:

  • The history of oil use, including predictions about the future
  • The chemistry of crude oil
  • Exploration for and production of oil
  • Refining
  • Petrochemicals
  • Transporting oil
  • Storing oil
  • Seasonal demand variation, pricing, and oil markets

Downey covers each in a clear and informative manner, though he sometimes delves into a greater level of detail than most amateurs will prefer. For instance, some of the forays into chemistry are at a level of sophistication well above what casuals readers are likely to retain. That said, the book is laid out in a highly structured way, so it is easy to gloss over technical portions without losing track of the overall structure of the text.

One thing the book strongly demonstrates is the enormous amount of expertise and capital that have been developed within the petroleum industry. For instance, the section on how offshore oil platforms are constructed and operated shows what an astonishing number of things can be executed deep underground, from a steel platform above the ocean’s surface: everything from horizontal and vertical drilling to the assembly of steel pipes (cemented in place), the use of explosives, the installation of automatic or remote-controlled valves, the injection of acids and chemicals, etc. The discussion of refining and transport technologies and infrastructure is similarly demonstrative of sustained investment and innovation. While it is regrettable that all of this effort has been put into an industry that is so climatically harmful, it does suggest that humanity has a great many physical and intellectual resources to bring to bear on the problem of finding energy. As more and more of those are directed towards the development of renewable energy options, we have reason to hope that those technologies will improve substantially.

The final portion of the book, about oil prices and forward oil markets, was the least interesting for me, as it deals with complex financial instruments rather than matters of chemistry, geology, etc. Still, for those who are seeking to understand how oil prices are established, as well as what sorts of financial instruments exist that relate to hydrocarbons, these chapters may be useful. Downey does provide some practical advice to those whose organizations (companies, countries, etc) are exposed to changes in oil markets: “The decision not to hedge [Buy financial products that reduce your exposure to a risk of major price changes] should be an active decision. Management should clearly inform investors why they decide to face the full volatility of the oil market when they have an opportunity to manage the risk.” Managing such risks on an individual level has been discussed here before.

All told, this book is well worth reading for all those who are curious about the energy basis for global civilization, why it is established the way it is, and some of the key factors that will determine which way it goes. Downey is a low-key proponent of the peak oil theory. He argues that reserves, especially in OPEC, are inflated and that a peak and bell-shaped drop-off in production are inevitable: probably between 2005 and 2015, provided depletion occurs globally at about the same rate as it did in the United States following their peak in 1970. For those hoping to grasp the implications of that projection, as well as those hoping to plan for a world based on other forms of energy, the information contained in this book is both valuable and well-presented.

British, EU, and US negotiators expect little from Copenhagen

Apparently, the United States has now made clear that they do not expect a climate deal to emerge at Copenhagen this year, when the United Nations Framework Convention on Climate Change (UNFCCC) gathering is to take place. This isn’t really news, but it is certainly disappointing. In a few years, I think people will look back regretfully at how much time, money and political energy were directed at the credit crunch, while the much more important problem of climate change mitigation was neglected.

A big part of the reason for the delay is certainly the difficulty the Obama administration has had getting a climate change bill through Congress. The Republicans deserve a lot of criticism for their caveman mentality on this issue. Their united opposition to meaningful action on climate change is irresponsible and a dereliction of duty, insofar as they are charged with defending the long-term welfare of the United States. While pricing carbon will cause short-term harm to certain industries now, it is the only way to kick off the sustained transition to a low-carbon economy that long-term prosperity ultimately depends upon.

Cruise ship size record reset

At the end of October, the MS Oasis of the Seas was launched in Finland. It is the world’s largest cruise ship, 360 metres long, with capacity for 6,296 passengers. In November of next year, a second ship of the same class is expected to be launched: the MS Allure of the Seas. The ship is powered by three 13.9 megawatt (MW) engines and three 18.5 MW engines, with propulsion from three 20 MW Azipods.

I cannot help but think that if the advocates of the peak oil hypothesis are correct, these vessels will end up being viewed as the height of fossil-driven folly. The ship is also a reminder of how international waters remain the part of the planet with the most lax environmental standards, whether the pollutant in question is sulphur dioxide, carbon dioxide, or anything else. Indeed, large oceangoing vessels generally need to carry two types of fuel: one that is legal for use in the domestic waters of states with air pollution laws, and another that can only be used on the open ocean.

Octane and gasoline engines

Smashed wooden wall

I am learning a lot about hydrocarbon fuels from Morgan Downey’s Oil 101. For instance, that the common understanding of the phrase ‘high octane’ is somewhat misleading. In the context of gasoline-powered internal combustion engines, such as those in cars, the octane rating of a fuel refers to how much it can be compressed along with air before it will spontaneously ignite. In these engines, fuel and air are mixed together and compressed in a cylinder. They are then ignited at a precisely controlled time by a spark plug. Cases where the mixture explodes before then are called ‘engine knock’ and are damaging. As such, engines are designed to use fuel above a certain octane number, in order to be confident that knocking will not occur.

When it comes to choosing fuel to buy, this means it is appropriate to use a grade with an octane rating as high as cited in the operating manual of a vehicle. Going higher, however, may be a waste of money for two independent reasons. Firstly, higher octane fuels are more expensive because they cost more for refineries to produce. Unless your engine is tuned to take advantage of the extra opportunity for compression, no additional power will be generated. Secondly, higher octane fuels often contain less energy per litre, because the hydrocarbons that comprise them have less energy in their chemical bonds. As such, a litre of more-expensive high octane fuel likely will not take a vehicle as far as a cheaper litre of adequate-octane fuel.

Octane numbers are assigned based on how a fuel compares to two specific hydrocarbons: isooctane (which is hard to ignite by compression) and n-heptane (which is easy to ignite that way). 90 octane fuel is thus as resistant to pressure-induced ignition as a mixture of 90% isooctane and 10% n-heptane. Some fuels are even better at resisting pressure-induced ignition than isooctane, and can therefore have octane numbers over 100.

In diesel engines, this is reversed. They do not have spark plugs and rely upon the ability of fuel to ignite spontaneously in the presence of pressurized air. In diesel, the cetane number refers to the propensity of fuel to autoignite on compression. Here, a higher number is more desirable.

One other thing I didn’t know about liquid transport fuels is that the fuel used by piston-driven aircraft, such as small propeller planes, still uses tetra ethyl lead to increase its octane rating. This practice has been discontinued in cars both because it interferes with catalytic converters and because it was massively increasing human exposure to lead – a known cause of brain damage. In aviation gasoline, tetra ethyl lead is used instead of alcohols to boost octane. This is because alcohol-blended fuels are less energy dense, more prone to vapour lock, liable to separate at low temperatures, as vulnerable to corrosion. Such aircraft are a relatively tiny share of the total market for hydrocarbon fuels; still, it isn’t particularly comforting to know that they continuously disperse lead on whatever is below them.

Fighting oil sands emissions by burning natural gas?

According to Morgan Downey’s Oil 101, it actually takes more energy to produce a barrel of synthetic crude oil from the oil sands than the barrel of crude contains. Most of that extra energy comes from natural gas. It is worth paying that energy cost because crude oil is a valuable product that can be turned into gasoline, kerosene, etc, whereas unprocessed bitumen laden sand has no value. Note that even more energy is required to run the refineries that turn synthetic crude into usable fuels.

As a result of this, the economic viability of the oil sands depends on natural gas remaining cheap enough for synthetic crude to compete. As such, it is arguably the case the promoting natural gas as a fuel for vehicles and electricity generation is a smart climatic move. It is a relatively clean fuel in those applications, and using it in that way might keep a larger share of it from being used to upgrade bitumen – thus leaving the carbon contained therein safely buried.

In Scenario A (cheap gas), a lot of Canada’s northern natural gas goes towards liquefying and upgrading bitumen, thus liberating the carbon it contains into the atmosphere, both during upgrading and refining processes and when the resultant fuels are burned.

In Scenario B (expensive gas), the natural gas is used for higher-value purposes like electricity generation, and more of the carbon in the bitumen never ends up in the atmosphere. Other forms of environmental damage associated with the oil sands – including air and water pollution, habitat destruction, etc – are also lessened.