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International CO2 emissions control: An analysis using CETA

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Abstract

This paper explores issues of international cooperation in CO2 emission control. We consider three cases: ‘selfish,’ in which region 1 controls optimally given its own damage costs and region 2 does not control; ‘altruistic,’ in which region 1 controls optimally given total worldwide damage costs while region 2 does not control; and ‘optimal,’ in which regions 1 and 2 exercise jointly optimal control of emissions and region 1 pays region 2 to participate. We find that neither region gains much in the selfish case; but both regions are better off in the optimal case than in the altruistic case, though region 1's benefits are negative in both these cases.

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We present an economic growth and energy use model incorporating representations of greenhouse gas accumulation, global mean temperature rise, and the damage cost associated with this temperature rise. Under alternative assumptions about the damage cost function, we find optimal time paths of CO, emissions control and associated optimal carbon taxes. Our work indicates that with plausible assumptions, an optimal carbon tax will rise over time, in contrast to the "hump shaped" carbon taxes implied by C02 reduction policies currently being discussed. Our work also suggests that the damage cost function would have to be both high and nonlinear in order to justify the general level of CO2 control and carbon taxes implied by these policies.
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Inorganic carbon in the ocean is modelled as a passive tracer advected by a three-dimensional current field computed from a dynamical global ocean circulation model. The carbon exchange between the ocean and atmosphere is determined directly from the (temperature-dependent) chemical interaction rates in the mixed layer, using a standard CO2 flux relation at the air-sea interface. The carbon cycle is closed by coupling the ocean to a one-layer, horizontally diffusive atmosphere. Biological sources and sinks are not included. In this form the ocean carbon model contains essentially no free tuning parameters. The model may be regarded as a reference for interpreting numerical experiments with extended versions of the model including biological processes in the ocean (Bacastow R and Maier-Reimer E in prep.) and on land (Esser G et al in prep.). Qualitatively, the model reproduces the principal features of the observed CO2 distribution bution in the surface ocean. However, the amplitudes of surface pCO2 are underestimated in upwelling regions by a factor of the order of 1.5 due to the missing biological pump. The model without biota may, nevertheless, be applied to compute the storage capacity of the ocean to first order for anthropogenic CO2 emissions. In the linear regime, the response of the model may be represented by an impulse response function which can be approximated by a superposition of exponentials with different amplitudes and time constants. This provides a simple reference for comparison with box models. The largest-amplitude (0.35) exponential has a time constant of 300 years. The effective storage capacity of the oceans is strongly dependent on the time history of the anthropogenic input, as found also in earlier box model studies.
Article
For national environmental problems, appropriately designed emission taxes lead to efficient outcomes. The paper gives an analysis of the properties of an international tax on CO2 emissions. A uniform CO2 tax for all countries does not necessarily give the first best social optimum. In practice, however, a uniform tax at an appropriate level will give an allocation of emissions which is very close to the allocation in the first-best optimum. CO2 emissions affect the climate through cumulative emissions. In a dynamic game of CO2 emissions, it is shown that the tax giving a Pareto optimal solution is the same for the open loop and the perfect equilibrium, in spite of the fact that these two equilibria differ in the absence of a CO2 tax.
Article
In this paper, we investigate the sensitivity of optimal carbon control strategies to parameters of the Carbon Emissions Trajectory Assessment (CETA) Model, and we use CETA in a simple decision tree framework to estimate the value of information about global warming uncertainties. We find that if an optimal control policy is used under uncertainty, the eventual resolution of uncertainty has high value relative to current research budgets, and resolving uncertainty about the costs of warming is nearly as important as resolving uncertainty about the extent of warming. In addition, we find that there is not a high premium on immediate resolution of uncertainty, if resolution would otherwise occur within, say, twenty years; this implies that time is available to plan and execute a carefully designed research program. On the other hand, we find that if the real world political process would result in a suboptimal control policy being chosen under uncertainty, and this choice could be prevented by early resolution of uncertainty, the benefit of early resolution may be as much as three orders of magnitude greater.
Article
Economic analyses of efficient policies to slow climate change require combining economic and scientific approaches. The present study presents a dynamic integrated climate-economy (‘DICE’) model. This model can be used to investigate alternative approaches to slowing climate change. Evaluation of five policies suggest that a modest carbon tax would be an efficient approach to slow global warming, while rigid emissions-stabilization approaches would impose significant net economic costs.
Article
We use a global model to compare the economic performance of three policy instruments for controlling CO2 emissions — period specific emission limits (limit policy), period specific taxes (tax policy), and a cumulative emissions limit (cumulative limit policy). With known costs and benefits of control, tax and limit policies are equivalent, and either is better than a cumulative limit policy. With uncertain benefits of emission reduction, tax and limit policies are equivalent. However, with uncertain costs of emission reduction, a tax policy may be better. A cumulative limit policy may occasionally perform well under uncertainty, but this is not generally the case.
Article
Human activity this century has increased the concentrations of atmospheric trace gases, which in turn has elevated global surface temperatures by blocking the escape of thermal infrared radiation. Natural climate variations are masking this temperature increase, but further additions of trace gases during the next 65 years could double or even quadruple the present effects, causing the global average temperature to rise by at least 1 °C and possibly by more than 5 °C. If the rise continues into the twenty-second century, the global average temperature may reach higher values than have occurred in the past 10 million years.
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CO2 emissions control: comparing policy instruments
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Contribution of different greenhouse gases to global warming: a new technique for measuring impact
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