Risk Communication on Climate

John Sterman’s new Policy Forum in Science should be required reading. An excerpt:

The strong scientific consensus on the causes and risks of climate change stands in stark contrast to widespread confusion and complacency among the public. Why does this gulf exist, and why does it matter? Policies to manage complex natural and technical systems should be based on the best available scientific knowledge, and the Intergovernmental Panel on Climate Change (IPCC) provides rigorously vetted information to policy-makers. In democracies, however, the beliefs of the public, not only those of experts, affect government policy.

Effective risk communication is grounded in deep understanding of the mental models of policy-makers and citizens. What, then, are the principal mental models shaping people’s beliefs about climate change? Studies show an apparent contradiction: Majorities in the United States and other nations have heard of climate change and say they support action to address it, yet climate change ranks far behind the economy, war, and terrorism among people’s greatest concerns, and large majorities oppose policies that would cut greenhouse gas (GHG) emissions by raising fossil fuel prices.

More telling, a 2007 survey found a majority of U.S. respondents (54%) advocated a “wait-and-see” or “go slow” approach to emissions reductions. Larger majorities favored wait-and-see or go slow in Russia, China, and India. For most people, uncertainty about the risks of climate change means costly actions to reduce emissions should be deferred; if climate change begins to harm the economy, mitigation policies can then be implemented. However, long delays in the climate’s response to anthropogenic forcing mean such reasoning is erroneous.

Wait-and-see works well in simple systems with short lags. We can wait until the teakettle whistles before removing it from the flame because there is little lag between the boil, the whistle, and our response. Similarly, wait-and-see would be a prudent response to climate change if there were short delays in the response of the climate system to intervention. However, there are substantial delays in every link of a long causal chain stretching from the implementation of emissions abatement policies to emissions reductions to changes in atmospheric GHG concentrations to surface warming to changes in ice sheets, sea level, agricultural productivity, extinction rates, and other impacts. Mitigating the risks therefore requires emissions reductions long before additional harm is evident. Wait-and-see policies implicitly presume the climate is roughly a first-order linear system with a short time constant, rather than a complex dynamical system with long delays, multiple positive feedbacks, and nonlinearities that may cause abrupt, costly, and irreversible regime changes.

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Climate, the Bailout, and the Blame Game

I’ve been watching a variety of explanations of the financial crisis. As a wise friend noticed, the only thing in short supply is acceptance of responsibility. I’ve seen theories that place the seminal event as far back as the Carter administration. Does that make sense, causally?

In a formal sense, it might in some cases. I could have inhaled a carcinogen a decade ago that only leads to cancer a decade from now, without any outside triggers. But I think that sort of system is a rarity. As a practical matter, we have to look elsewhere.

Socioeconomic systems are at a constant slow boil, with many potential threats existing below the threshold of imminent danger at any given time. Occasionally, one grows exponentially and emerges as a real catastrophe. It seems like a surprise, because of the hockey stick behavior of growth (the French riddle of the lily pond again). However, most apparent low-level threats never emerge from the noise. They don’t have enough gain to grow fast, or they get shut down by some unsuspected negative feedback.

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Dimensions of The Deal

In the Tällberg event we talked a lot about the deal we need, without really defining what was meant by that. I think it has at least four dimensions:

Technical

What science drives the goal? Is it 350ppm? 450ppm? 550ppm? 2C?

Social

What regions or sectors will move first, and what transfers will the rich or the winners use to induce the poor or the losers to play along? Do transfers consist of money, intellectual property, or both?

Implementation

What form will commitments take, who will make them, and how will they be implemented? Will the mechanism favor taxes or trading, for example? Will standards be expressed as intensities or absolute emissions or … ? How will goals and mechanisms adapt as we learn about uncertainties?

Coalition

We don’t have a deal now because we don’t have the coalition needed to make it happen. Some combination of the public, politicians, media, religion, education, etc. needs to come together to create critical mass behind a policy. We have fragments (the EU, California) but not a whole. I rather doubt that there is a quick, transformative solution (unless catastrophe drives us to one, which I’d rather not contemplate).

I say “critical mass” deliberately, because what we’re all implicitly searching for is a reinforcing feedback that will grow policy out of its current dysfunctional state. The question is, what is that loop? My guess is that it involves starting gradually. Don’t shoot for the moon and fail. Instead, take a little medicine at first. Impose a modest carbon tax. Observe that the economy doesn’t collapse, and efficiency is cheap or even profitable. Greentech gets a little more profitable, and the more numerous low-carbon voters grow to enjoy their tax rebates. Enlisting their support allows the tax to be ratcheted up further, and soon you’re rolling toward real emissions controls. But is the gain on that loop high enough to yield emissions reductions in time to avoid catastrophe?

Hansen on The Deal

Jim Hansen kicked off the Tällberg panel with a succinct summary of the argument for a 350ppm target in Hansen et al. (a short version is here). As I heard it,

  • The dangerous level of GHGs in the atmosphere is lower than we thought.
  • 3C climate sensitivity from fast feedbacks is confirmed; the risk is slow feedbacks, which are not as slow as we thought.
  • There is enough warming in pipeline to lose arctic ice, glaciers, reefs.
  • Good news: we need to go back to the stable Holocene climate.
  • The problem is solvable because conventional oil and gas are limited; we just need the will to not burn coal, oil shale, etc., except with CCS.
  • Among other things, that requires a price on carbon; for which a tax is the preferred mechanism.
  • The only loser is the fossil fuel industry; we simply need to bring them to heel.

Hansen was a little impatient with our bit of the forum, and argued that our focus on regions (and the challenges in reaching a regional accord) was too pessimistic. Instead, a focus on fuels (e.g., phasing out coal) provides clarity of purpose.

My counterargument, which I only partially articulated during the session, for fear of driving the conversation off on a tangent, is as follows:

As a technical solution, phasing out coal and letting peak oil run its course probably works. However, phasing out coal by 2030 implies a time constant of seven years or a rate of decline in coal utilization of about 10%/year (by the 3-tau rule of thumb). Coal-fired power plants have a long lifetime, so the natural rate of decline, assuming no new coal investment, is more like 2.5% or 3%/year. Phasing out coal at 10% per year implies not only halting construction, but also abandoning many plants before their natural economic lifetime is up. Age structure complicates things a bit, perhaps making it easier in the US (where plants are disproportionately old) and harder in China (where they’re new). Closing plants ahead of schedule is going to make the fossil fuel interests that Hansen proposes to control rather vocally upset. Also, eliminating coal emissions that fast requires some combination of rapid deployment of efficiency, noncarbon energy sources, and CCS above natural rates of capital turnover, and lifestyle change to pick up the slack. That in itself is a significant challenge.

That would be doable for a coalition with enough political power to either overpower or buy off the owners of stranded assets. But that coalition doesn’t now exist, and therein lies the reason that this is a political problem more than a technical one.

Tol Talks Tax

Stumbled upon while searching for a reference: Richard Tol Changes Tune, Talks Carbon Tax. From what I’ve read, Tol is too much of a nonconformist to club with the professional skeptics, and has probably always preferred a Hotelling-style carbon price trajectory, so I’m not convinced that this is really a change, but it’s intriguing.

Aviation Pontification

Last week I presented in an INFORMS 2008 panel, Role Reversal: The Impact of Climate Change on Aviation. My slides are here (you’ll miss a model demo using a carbon cycle/climate model, but that wasn’t central). I got challenged on one assertion – that participation in regional initiatives is meaningful – on the grounds that federal preemption definitively assigns aviation regulation to the national level. That may be so, but I suspect that mental models formed through regional experimentation will still shape what happens nationally. Without early involvement, aviation could find itself getting pounded into the nearest available policy pigeonhole, regardless of fit. Avaitors joke that, “gravity never loses; the best you can hope for is a draw.” The same could perhaps be said of aviation’s chance of withstanding the inexorable consequences of GHG accumulation.

The Deal We Ain't Got

Today, Drew Jones and I presented a simple model as part of the Tällberg Forum’s Washington Conversation, ‘The climate deal we need.’ Our goal was to build from some simple points about the bathtub dynamics of the carbon cycle and climate to yield some insights about what’s needed. Our aspirational list of insights to get across included,

  • stabilizing emissions near current levels fails to stabilize atmospheric concentrations any time soon (because emissions now exceed uptake of carbon; stabilization continues that condition, and the residual accumulates in the atmosphere)
  • achieving stabilization of atmospheric CO2 at low levels (Hansen et al.’s 350 ppm) requires very aggressive cuts (for the same reason; if carbon cycle feedbacks from temperature kick in, negative emissions could be needed)
  • current policies are not on track to meaningful reductions (duh)
  • nevertheless, there is a path (Hansen et al.’s “where should humanity aim” paper lays out one option, and there are others)
  • starting soon is essential (the bathtub continues to fill while we delay – a costly gamble)
  • international negotiation dynamics are tricky due to diversity of interests, coupled problem spaces, and difficulty of transfers (simulations shadow this)
  • but everyone has to be on board or little happens (any one major region or sector, uncontrolled, can blow the deal by emitting above natural uptake)

A good moment came when someone asked, “Why should we care about staying below some temperature threshold?” (I think a scenario with about 3.5C was on the screen at the time). Jim Hansen answered, “because that would be a different planet.”

The conversation didn’t lead to specification of “the deal we need” but it explored a number of interesting facets, which I’ll relate in a few follow-on posts.

WCI Design Recommendations

Yesterday the WCI announced its design recommendations.

Update 9/26: WorldChanging has another take on the WCI here.
I haven’t read the whole thing, but here’s my initial impression based on the executive summary:

Scope

Major gases, including CO2, methane, nitrous oxide, hydrofluorocarbons, perfluorocarbons and sulfur hexafluoride.

What? In scope? How/where?
Large Industrial & Commercial, >25,000 MTCO2eq/yr

Combustion Emissions

Yes Point of emission

Process Emissions

Yes Point of emission
Electricity Yes “First Jurisdictional Deliverer” – includes power generated outside WCI
Small Industrial, Commercial, Residential Second Compliance Period (2015-2017) Upstream (“where fuels enter commerce in the WCI Partner jurisdictions, generally at a distributor. The precise point is TBD and may vary by jurisdiction”)
Transportation

Gasoline & Diesel

Second Compliance Period (2015-2017) Upstream (“where fuels enter commerce in the WCI Partner jurisdictions, generally at a terminal rack, final blender, or distributor. The precise point is TBD and may vary by jurisdiction”)

Biofuel combustion

No
Biofuel & fossil fuel upstream To be determined ?
Biomass combustion No, if determined to be carbon neutral  
Agriculture & Forestry No  

(See an earlier Midwestern Accord matrix here.)

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The GAO's Panel of Economists on Climate

I just ran across a May 2008 GAO report, detailing the findings of a panel of economists convened to consider US climate policy. The panel used a modified Delphi method, which can be good or evil. The eighteen panelists are fairly neoclassical, with the exception of Richard Howarth, who speaks the language but doesn’t drink the Kool-aid.

First, it’s interesting what the panelists agree on. All of the panelists supported establishing a price on greenhouse gas emissions, and a majority were fairly certain that there would be a net benefit from doing so. A majority also favored immediate action, regardless of the participation of other countries. The favored immediate action is rather fainthearted, though. One-third favored an initial price range under $10/tonCO2, and only three favored exceeding $20/tonCO. One panelist specified a safety valve price at 55 cents. Maybe the low prices are intended to rise rapidly (or at the interest rate, per Hotelling); otherwise I have a hard time seeing why one would bother with the whole endeavor. It’s quite interesting that panelists generally accept unilateral action, which by itself wouldn’t solve the climate problem. Clearly they are counting on setting an example, with imitation bringing more emissions under control, and perhaps also on first-mover advantages in innovation.

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Regional Climate Initiatives – Model Roll Call – Part II

Minnesota

The Minnesota Next Generation Energy Act establishes a goal of reducing GHG emissions by 15% by 2015, 30% by 2025, and 80% by 2050, relative to 2005 levels.

From ScienceDaily comes news of a new research report from University of Minnesota’s Center fro Transportation Studies. The study looks at options for reducing transport emissions. Interestingly, transport represents 24% of MN emissions, vs. more than 40% in CA. The study decomposes emissions according to a variant of the IPAT identity,

Emissions = (Fuel/VehicleMile) x (Carbon/Fuel) x (VehicleMilesTraveled)

Vehicle and fuel effects are then modeled with LEAP, an energy modeling platform with a fast-growing following. The VMT portion is tackled with a spreadsheet calculator from CCAP’s Guidebook. I haven’t had much time to examine the latter, but it considers a rich set of options and looks like at least a useful repository of data. However, it’s a static framework, and land use-transportation interactions are highly dynamic. I’d expect it to be a useful way to construct alternative transport system visions, but not much help determining how to get there from here.

Minnesota’s Climate Change Advisory Group TWG on land use and transportation has a draft inventory and forecast of emissions. The Energy Supply and Residential/Commercial/Industrial TWGs developed spreadsheet analyses of a number of options. Analysis and Assumptions memos describe the results, but the spreadsheets are not online.

British Columbia

OK, it’s not a US region, but maybe we could trade it for North Dakota. BC has a revenue-neutral carbon tax, supplemented by a number of other initiatives. The tax starts at $10/TonCO2 and rises $5/year to $30 by 2012. The tax is offset by low-income tax credits and 2 to 5% reductions in lower income tax brackets; business tax reductions match personal tax reductions in roughly a 1:2 ratio.

BC’s Climate Action Plan includes a quantitative analysis of proposed policies, based on the CIMS model. CIMS is a detailed energy model coupled to a macroeconomic module that generates energy service demands. CIMS sounds a lot like DOE’s NEMS, which means that it could be useful for determining near-term effects of policies with some detail. However, it’s probably way too big to modify quickly to try out-of-the-box ideas, estimate parameters by calibration against history, or perform Monte Carlo simulations to appreciate the uncertainty around an answer.

The BC tax demonstrates a huge advantage of a carbon tax over cap & trade: it can be implemented quickly. The tax was introduced in the Feb. 19 budget, and switched on July 1st. By contrast, the WCI and California cap & trade systems have been underway much longer, and still are no where near going live. The EU ETS was authorized in 2003, turned on in 2005, and still isn’t dialed in (plus it has narrower sector coverage). Why so fast? It’s simple – there’s no trading infrastructure to design, no price uncertainty to worry about, and no wrangling over allowance allocations (though the flip side of the last point is that there’s also no transient compensation for carbon-intensive industries).

Bizarrely, BC wants to mess everything up by layering cap & trade on top of the carbon tax, coordinated with the WCI (in which BC is a partner).